Showing posts with label My Project. Show all posts
Showing posts with label My Project. Show all posts

Monday, March 9, 2009

Lebuhraya Pantai Timur









Panjang = 169km

Tarikh dibuka = 01-Ogos-2004
Tarikh dibina = 30-Ogos-2000

Konsesi = MTD Capital Bhd.
Pemaju = MTD Capital Bhd.



Lebuhraya Pantai Timur (LPT) adalah Lebuhraya 4 lorong 2 hala yang menghubungkan Karak dalam negeri Pahang ke Chendering dalam negeri Terengganu melalui Kuantan. Ianya merupakan sambungan dari Lebuhraya Kuala Lumpur - Karak yang ada sekarang bermula dari Karak, Negeri Pahang (berhampiran dengan stesyen timbang JPJ sekarang) dan berakhir di Chendering, Negeri Terengganu melalui Lanchang, Mentakab, Temerloh, Chenor, Maran, Kuantan, Jabur, Bukit Besi, Ajil dan Chendering. Kerja pembinaan Lebuhraya ini sepatutnya bermula pada awal tahun 1999. Oleh kerana Syarikat terdahulu telah gagal membuat Perjanjian Konsesi 'effective', kerajaan telah membuat keputusan untuk membiayai sendiri projek ini secara 'turnkey contract', dimana pembinaannya terbahagi kepada dua fasa iaitu Fasa 1 (Negeri Pahang) dan Fasa 2 (Negeri Terengganu).

Fasa-fasa dalam pembinaan Lebuhraya Pantai Timur (LPT)

Fasa 1 : Negeri Pahang

Sebagai permulaan untuk merealisasikan projek ini Kerajaan telah memulakan Pembinaan Lebuhraya Pantai Timur Fasa 1 sepanjang 169 KM dimana ia adalah sambungan dari Lebuhraya Kuala Lumpur-Karak yang ada sekarang bermula di Karak dan berakhir di Kuantan sempadan Pahang-Terengganu dan menawarkan projek ini kepada MTD Capital Berhad sebagai kontrator 'turnkey'. Kerja-kerja pembinaan telah dimulakan pada bulan Ogos 2000 dengan kos pembinaannya ialah RM 1.3 billion atau RM 7.5 juta sekilometer.

Maklumat Kontrak

Pegawai Penyelia : Ketua Pengarah Lembaga lebuhraya Malaysia.
Kontraktor Turnkey : MTD Capital Bhd.
Jurutera Perunding : Terratech Consultants.

Fakta Teknikal
Laluan 4 lorong 2 hala dengan kelajuan rekabentuk 120 km/jam.
  • Beroperasi secara sistem tol tertutup.
  • Terdapat 52 buah jambatan melintasi sungai-sungai dan jalan-jalan sedia ada.
  • Stesyen timbang JPJ (3 unit) iaitu: 1. Kg. Bintang, 2. Paya Rambutan, 3. FELDA Panching Timur
  • Kawasan Rehat dan Rawat (R&R) (4 unit) iaitu (2 unit) di Kg. Bintang dan (2 unit) di Paya Rambutan.
  • Hentian Sebelah (Layby) (6 unit) iaitu (2 unit) di FELDA Lakum, (2 unit) di FELDA Bukit Tajau dan ( 2 unit) di FELDA Pancing Timur.
  • Terdapat 85 buah VBC (Vehicular Box Culvert) untuk kemudahan penduduk kampung melintasi lebuhraya.
  • Sebanyak 8 Persimpangan Bertingkat yang dibina dalam negeri Pahang iaitu:
  • 1. Persimpangan Bertingkat Karak.
  • 2. Persimpangan Bertingkat Lanchang.
  • 3. Persimpangan Bertingkat Temerloh.
  • 4. Persimpangan Bertingkat Chenor.
  • 5. Persimpangan Bertingkat Maran.
  • 6. Persimpangan Bertingkat Sri Jaya.
  • 7.Persimpangan Bertingkat Gambang.
  • 8. Persimpangan Bertingkat Kuantan
Lebuhraya Pantai Timur Fasa 1 telah dibuka kepada orang pada 1 Ogos 2004 dimana ia telah diramikan oleh Kebawah Duli Yang Maha Mulia Sultan Pahang, bertempat di Plaza Tol Kuantan. Pengguna akan dikenakan bayaran tol bermula pada 3 September 2004 bersamaan dengan hari Jumaat


Fasa 2 : Negeri Terengganu

Terdapat perubahan terhadap cadangan jajaran bagi mengambil kira aspek teknikal dan sosial dan untuk mengelakkan kesesakan di Bandar Kuala Terengganu di mana Lebuhraya berakhir di Sg. Tong Kuala Terengganu. Pada masa ini pembinaan belum dijalankan.Dengan terlaksananya projek ini ianya akan menjadi penghubung darat yang utama antara koridor di pantai barat dan pantai timur. Ianya juga akan memendekkan masa perjalanan dari pantai barat ke timur.


Lebuhraya Pantai Timur (LPT) yang berharga RM1.2billion ini ialah sensasi terkini sector pengangkutan awam di Malaysia. LPT dibuka kepada orang ramai pada 1 Ogos 2004. Rakyat dipelawa menguji lebuhraya ini selama satu bulan tanpa tol. LPT sangat signifikan kerana ianya adalah satu-satunya lebuhraya 4-lorong yang menghubungkan pantai barat dan pantai timur Semenanjung Malaysia. LPT diharapkan dapat memacu pembangunan ekonomi di wilayah pantai Timur Semenanjung Malaysia.

Projek LPT dilaksanakan dalam 2 fasa. Fasa 1 menghubungkan Karak ke Kuantan, PAHANG. Fasa 2 menghubungkan Kuantan ke Kuala Terengganu, TERENGGANU.

Fasa 1 Lebuhraya sepanjang 169 km ini bermula di Karak, Pahang (persimpangan Karak) dan berakhir di sempadan Pahang/Terengganu (persimpangan Kuantan). Ianya merupakan sambungan dari Lebuhraya Kuala Lumpur - Karak yang ada sekarang.

LPT juga terkenal dengan kadar kemalangan yang tinggi. Sejak dibuka pada Ogos lalu, sebanyak 108 kemalangan yang telah berlaku di LPT. Laporan pakar menunjukkan antara faktor penyebabnya ialah kerosakan pada rekabentuk di km36 lebuhraya itu yang menyebabkan sesetengah kenderaan laju "menggelungsur" di sudut jalan. Ini berlaku kerana penaikan tinggi tidak mencukupi antara sepanjang jalan Km90 dan Km126. MTD Capital Bhd selaku kontraktor turnkey diarahkan membetulkan segala kecacatan rekabentuk LPT. Susur Keluar (Exits)


Terdapat 8 susur keluar dari LPT melalui 8 persimpangan bertingkat, iaitulah Karak, Lanchang, Temerloh, Chenor, Maran, Sri Jaya, Gambang dan Kuantan. (lihat peta di atas). Jarak persimpangan antara Temerloh dan Chenor paling dekat hanya dipisahkan oleh Sungai Pahang.
Setiap susur keluar mempunyai lampu jalan “floodlight’ yang mencukupi. Jambatan merentasi Sungai Pahang dihiasi lampu yang berlebihan.

Kemudahan-kemudahan asas

Terdapat 4 kawasan Rehat dan Rawat (R&R) dan 6 hentian sebelah (lay-by) di sepanjang LPT. Kawasan rehat mempunyai kemudahan bilik air, gerai-gerai makanan/minuman dan surau. Pemandu-pemandu yang mengantuk boleh tidur sekejap di hentian sebelah.
Stesen-stesen minyak boleh dijumpai di setiap kawasan rehat (2 Shell dan 2 Petronas). Pada waktu kembara ini, hanya kawasan rehat Temerloh yang dibuka sepenuhnya.

Had Laju

Had laju di kebanyakan bahagian ialah 110 km/j. Sebahagian laluan mempunyai had laju 90km/j disebabkan risiko selekoh, jalan tidak rata dan angin lintang (cross wind). Kereta berkeupayaan tinggi bergerak selesa pada kelajuan 150km/j tetapi tidak digalakkan.


Kadar Tol

Kadar tol dari persimpanagan Karak ke persimpangan Gambang ialah RM16.70 dan lebih kurang RM20 jika anda keluar di persimpangan Kuantan.

Sunday, March 8, 2009

Stormwater Software - InfoWorks WS

Taken from http://www.wallingfordsoftware.com/products/infoworks_ws/



Overview

The key objective for all water supply and distribution organizations is the efficient and sustainable supply of high quality water. This should be provided at an acceptable pressure and with minimal leakage losses. This challenge is affected by weather conditions, stringent regulatory environments, security concerns and an increasingly aware consumer audience.

InfoWorks WS gives an accurate view of the performance of your network and assists with meeting your operational targets. An accurate all mains water supply model can identify infrastructure weaknesses, water quality incidents and other operational needs. The model can also be used to simulate emergency conditions and investigate solutions.

Example Applications

  • Assessment of supply to individual customer level
  • Investigation of supply deficiencies
  • Demand management
  • Design and implementation of drought management plans
  • Planning of capital investment programs
  • Critical link analysis
  • Scenario planning & fire flow analysis
  • Simulation of pollution incidents
  • Assessing source blending requirements
  • Water quality and chlorination assessment
  • Sedimentation analysis and mains flushing
  • Optimization of pumping systems
  • Optimization of system storage

Features and Benefits

The leading software solution integrating asset and business planning with water supply and distribution network modeling:-

1. Workgroup Model Management

  • Manages multiple modelers on multiple projects
  • Highly efficient workflow within the organization - saves time and money on each project
  • Supports both Local and Network Dongles for licence authentication
  • Flexible implementation approach, which can be tailored to current and future IT strategies
  • Controls access permissions to models by user login details
  • Model data and results are secure at all times


2. Data Integration

  • Seamless exchange of data and results to and from GIS and other third party applications
  • Import models and export results to any data source using InfoWorks Open Data Import/Export Centre
  • Import asset data directly from Microsoft databases (Excel / Access), Oracle databases, GIS, XML, and Geodatabases
  • Import models from Stoner, EPANET, AQUIS, and WATSYS/WaterMax
  • Interfaces with SCADA and data logging systems

3. Model Building Tools

  • Automatic inference of missing model data and assignment of pipe friction coefficeints from user defined and built in material libaries
  • Allows data flagging on all model data
  • Engineering validation checks ensure consistency with expected engineering values
  • Tracing tools to help identify, view and modify network connectivity and hydraulic boundries
  • Carry out network comparisons and apply differences to any network
  • Consolidates modeling data from multiple sources in one coherent interface
  • If no electronic data is available InfoWorks provides the tools for simple and flexible manual digitization
  • Automatic demand allocation from any geo referenced seed point data (customer point)
  • Demand Management
  • Realistic pump modeling
  • Flexible object controls

4. Powerful Hydraulic Simulation

  • Exceptionally fast, robust and efficient with large networks
  • Fully integrated additional simulation types
  • Water Quality and Sedimentation Modeling
  • Fire flow modeling
  • Critical Link Analysis
  • Unidirectional Flushing tool
  • Automated Optimization

5. Results Interpretation

  • Fully dynamic thematic displays with simulation replays in Plan View
  • Database grid reports for all results
  • Time varying graphical data
  • Time varying Longitudinal Sections with dynamic pressure levels and pressure rating for the pipe
  • 3D Terrain View for viewing ground surface of networks with ability to shade hill contours
  • Result comparision for multiple simulations
  • Custom SQL queries on data and results
  • Custom reports

Tuesday, March 3, 2009

Sungai Selangor





















































The Sg Selangor Basin covers an area of about 1,960 km sq., which is nearly a quarter (24.6%) of the total area of the State of Selangor, and approximately 70 km long and 30 km wide. The Basin is located to the north of Kuala Lumpur City, bounded by the Sg Klang Basin in the south and Sg Bernam Basin in the north, and encompasses the Districts of Gombak, Kuala Selangor and Hulu Selangor in 19 Mukims. The Basin is rich with natural and ecological systems. The upper Basin provides a green and pristine upland with unique flora and fauna while the downstream areas have the natural wonder, internationally known firefly colony at Kg Kuantan.


Rapid urbanization in the Sg. Selangor basin has resulted in many conflicting interests of water users and environmental problems. The control of both the quantity and quality of runoff is now being seen to be of major importance in basin management and its receiving waters. Key issues that beset the Basin include declining water quality in its rivers, encroachment into most of its riparian reserves, downstream flooding and significant loss of forest cover.

Sungai Selangor Basin
The ‘Selangor river basin’ is located in the state of Selangor, in the mid-western part of Peninsular Malaysia. Within Selangor state the study area encompasses parts of three districts: Kuala Selangor, Hulu Selangor and Gombak (figure 3).
In figure 2 the location of the Selangor river basin is indicated with a rectangle in the map of Peninsular Malaysia. Figure 3 shows an enlargement of the rectangle indicated in figure 2.

Sungai Langat

About Sungai Langat


Sungai Langat is 120km long and originates from the Main Range. It drains westward to the Straits of Malacca. The major tributaries of Sungai Langat are the Sungai Semenyih and Sungai Labu.



According to local history, Sungai Langat was the main source of communication and transportation between the locals and foreign traders during the early days. The locals would travel to the mouth of theriver where barter posts were set up to enable trade between them and the foreigners.




In the year 2000, the Selangor State Government and the Department of Environment (DOE) adopted Sungai Langat in an effort to preserve the river and to improve the river's water quality through extensive clean-up operations, controlling the discharge of effluents into the river as well as conducting frequent checks on the level of water quality.

The water quality for Sungai Langat is currently rated as Class IIB (suitable for recreational use without treatment), and this rating is targetted to be raised to Class IIA (suitable for use as water supply with conventional treatment) by the year 2004.



Sungai Langat Dam

















Dam capacity 33,785 million liters.

Treatment treatment plant (Sungai Langat WTP)

capacity = 386 million liters per day (mld). Area

served : Hulu Langat, Cheras.


Lembangan Sungai Langat meliputi Negeri Selangor, Putrajaya serta sebahagian kecil Negeri Sembilan dan Wilayah Persekutuan Kuala Lumpur. Luas kawasan Lembangan Sungai Langat adalah 2,423 km2 (lembangan sungai yang terbesar di Selangor).Panjang Sungai Langat adalah 200 km.




PBT di dalam Lembangan Sungai Langat:

· Majlis Perbandaran Kajang (MPKj)
· Majlis Perbandaran Sepang (MPSp)
· Majlis Daerah Kuala Langat (MDKL)
· Majlis Perbandaran Ampang Jaya (MPAJ)
· Majlis Perbandaran Subang Jaya (MPSJ)
· Majlis Perbandaran Nilai
· Perbadanan Putrajaya (PPj)


Tiga buah anak sungai utama:


· Sg Semenyih (236 km2)
· Sg Labu (220 km2)
· Sg Beranang (325 km2)



Anak-anak sungai yang lain:

· Sg Mersing
· Sg Pangsoon
· Sg Lolo
· Sg Lopo
· Sg Congkak
· Sg Perdek
· Sg Lui
· Sg Semungkis
· Sg Gahal
· Sg Tekali
· Sg Michu
· Sg Sub
· Sg Betong
· Sg Serai
· Sg Perimbum
· Sg Raya
· Sg Cheras
· Sg Long
· Sg Sekamat
· Sg Balak
· Sg Merbau
· Sg Jeloh
· Sg Ramal
· Sg Rekoh
· Sg Jenderam
· Sg Chua
· Sg Belus
· Sg Semarang
· Sg Batang Nilai
· Sg Batang Benar
· Sg Jijan
· Sg Cincang
· Sg Salak
· Sg Air Hitam
· Sg Tekala
· Sg Batangsi
· Sg Saringgit
· Sg Rinching
· Sg Beranang Sg Kabul


Langat Basin



Langat Basin is located in south of Selangor and north of Negeri Sembilan within latitude 2"40'U to 3"20'U and longitude 101"10'E to 102"00'E with the geographical area extent of around 2,394.38 km2 (Figure 1).

















Geographical properties:

Longitude at River Outlet: 101° 17´ and 101° 58´ E
Latitude at River Outlet: 2° 44´ and 03° 16´ N
Area of River Basin: 2938 km2
Length of River: 120 km long
Altitude Range: 914 m
Average Annual Rainfall: 2469 mm or 1521–2883 mm
Average Rain days: 190
Average Temperature: 32° C
Average Humidity: 80%



The Langat River Basin is separated from Klang River Basin in the north, south and east by a series of highland ranges where the highest points are at Bukit Arang (560 m), Bukit Batu Bulan (1,008 m), Bukit Resam Ambat (1,149 m), Bukit Hitam (1,210m), Bukit Sebarau Chinchang (949 m), Bukit Angkau (1,055 m) Genting Jemelot (916 m), Bukit Sg. Puteh (409 m), Bukit Cennang (820 m) and Nuang Mountain (1,493 m). The average height of the highland ranges is about 960 meters (Anon, 1998). [Please note that the Malaysian terms of ‘bukit’ means hill and ‘gunung’ means mountain].
Demographic properties:

General location of the basin:
The Langat River Basin lies in the mid western part of Peninsular Malaysia and involves two states viz. Selangor State and Negeri Sembilan State, part of the Klang River Valley and now also includes the Putrajaya Federal Government Administrative Center. In Selangor it spans the districts of Sepang, Hulu Langat and Kuala Langat. In Negeri Sembilan it spans four mukims (sub district) of the western portion of the district of Seremban, namely Seremban, Labu, Lenggeng and Setul.

Total population in the Langat Basin was 1,184,917 million in 2000.

Sunday, March 1, 2009

Wet Pond

Taken from http://www.stormwatercenter.net/Assorted%20Fact%20Sheets/Tool6_Stormwater_Practices/Pond/Wet%20Pond.htm



Description

Wet ponds (a.k.a. stormwater ponds, retention ponds, wet extended detention ponds) are constructed basins that have a permanent pool of water throughout the year (or at least throughout the wet season). Ponds treat incoming stormwater runoff by settling and algal uptake. The primary removal mechanism is settling while stormwater runoff resides in the pool. Nutrient uptake also occurs through biological activity in the pond. Wet ponds are among the most cost-effective and widely used stormwater treatment practices. While there are several different versions of the wet pond design, the most common modification is the extended detention wet pond, where storage is provided above the permanent pool in order to detain stormwater runoff in order to provide greater settling.
Applicability

Wet ponds are a widely applicable stormwater treatment practice. While they may not always be feasible in ultra-urban areas or arid climates, they otherwise have few restrictions on their use.

Regional Applicability
Wet extended detention ponds can be applied in most regions of the United States, with the exception of arid climates. In arid regions, it is difficult to justify the supplemental water needed to maintain a permanent pool because of the scarcity of water. Even in semi-arid Austin, TX one study found that 2.6 acre-feet per year of supplemental water were needed to maintain a permanent pool of only 0.29 acre-feet (Saunders and Gilroy, 1997). Other modifications and design variations are needed in semi-arid and cold climates, and karst (i.e., limestone) topography (for more information see Stormwater Strategies for Arid and Semiarid Watersheds , Article 66 in the Practice of Watershed Protection and Performance of Stormwater Ponds in Central Texas, Article 74 in the Practice of Watershed Protection).

Ultra Urban Areas
Ultra urban areas are densely developed urban areas in which little pervious surface exists. It is difficult to use wet ponds in ultra urban areas because enough land area may not be available for the pond. Wet ponds can, however, be used in an ultra-urban environment if a relatively large area is available downstream of the site.

Stormwater Hotspots
Stormwater hotspots are land use or activities that generate highly contaminated runoff that has pollutant concentrations that exceed those typically found in stormwater. A typical example is a gas station or convenience store. Wet ponds can accept runoff from stormwater hotspots, but need significant separation from groundwater if they are used to treat hotspot runoff.

Stormwater Retrofit
A stormwater retrofit is a stormwater treatment practice (usually structural) put into place after development has occurred, to improve water quality, protect downstream channels, reduce flooding, or meet other watershed restoration objectives. Wet ponds are widely used for stormwater retrofits, and have two primary applications as a retrofit design. In many communities, dry detention ponds have been designed for flood control in the past. It is possible to modify these facilities to develop a permanent wet pool to provide water quality treatment (see "Treatment" under Design Considerations), and modify the outlet structure to provide channel protection. Alternatively, new wet ponds may be installed in streams, or in open areas as a part of a comprehensive watershed retrofit inventory.
Cold Water (Trout) Streams
Wet ponds pose a risk to cold water streams because of their potential to warm streams. When water remains in the permanent pool, it is heated by the sun. A study in Prince Georges County, MD found that wet ponds increased temperatures by about 9 F from the inlet to the outlet (Galli, 1990).
Siting and Design Considerations

Siting ConsiderationsDesigners need to ensure wet ponds are feasible for the site in question. The following section provides basic guidelines for locating wet ponds.

Drainage Area
Wet ponds need sufficient drainage area to maintain a permanent pool. In humid regions, a drainage area of about twenty-five acres is typically needed, but greater drainage areas are needed in arid and semi-arid regions.

Slope
Wet ponds can be used on sites with an upstream slope up to about 15%. The local slope within the pond should be relatively shallow, however. While there is no minimum slope requirement, there must be enough elevation drop from the pond inlet to the pond outlet to ensure that water can flow through the system by gravity.

Soils /Topography
Wet ponds can be used in almost all soils and geology, with minor design adjustments for regions of karst topography (see Design Considerations).

Groundwater
Unless they receive hotspot runoff, ponds can often intersect the groundwater table. However, some research suggests that pollutant removal is moderately reduced when groundwater contributes substantially to the pool volume (Schueler, 1997) (for more information, see Influence of Groundwater on Performance of Stormwater Ponds in Florida, Article 78 in The Practice of Watershed Protection.

Design Considerations
There are some design features that should be incorporated into all wet pond designs (see Figure 1). These design features can be divided into five basic categories: pretreatment, treatment, conveyance, maintenance reduction, and landscaping (for more information, see the Manual Builder Category).

Pretreatment
Pretreatment features are designed to settle out coarse sediment particles before they reach the main pool. By trapping these sediments in the forebay, it is possible to greatly reduce the maintenance burden of the pond. A sediment forebay is a small pool (typically about 10% of the volume of the permanent pool) located near the pond inlet. Coarse sediments are trapped in the forebay, and these sediments are removed from the smaller pool on a five to seven year cycle.

Treatment
Treatment design features help enhance the ability of a stormwater treatment practice to remove pollutants. Several features can enhance the ability of wet ponds to remove pollutants from stormwater runoff. The purpose of most of these features is to increase the amount of time that stormwater remains in the pond.

One technique to increase pond pollutant removal is to increase the volume of the permanent pool. Typically, ponds are sized to be equal to the water quality volume (i.e., the volume of water treated for pollutant removal). Designers may consider using a larger volume to meet specific watershed objectives, such as phosphorous removal. Regardless of the pool size, designers need to conduct a water balance analysis to ensure that sufficient inflow is available to sustain a permanent pool.

Other design features can increase the amount of time stormwater remains in the pond, and help to eliminate short circuiting. Wet ponds should always be designed with a length to width ratio of at least 1.5:1. In addition, the design should incorporate features to lengthen the flow path through the pond, such as underwater berms designed to create a longer flow path through the pond. Combining these two measures helps ensure that the entire pond volume is used to treat stormwater. Another feature that can improve treatment is to use multiple ponds in series as part of a "treatment train" approach to pollutant removal. This redundant treatment can also help slow the rate of flow through the system.

Conveyance
Stormwater should be conveyed to and from all wet ponds safely and to minimize downstream erosion potential. The outfall of pond systems should always be stabilized to prevent scour. In addition, an emergency spillway should be provided to safely convey large flood events. In order to prevent warming at the outlet channel, designers should provide shade around the channel at the pond outlet.

Maintenance Reduction
Several design features can be incorporated to ease the maintenance burden of wet ponds. Maintenance reduction features include techniques to reduce the amount of maintenance needed, as well as techniques to make regular maintenance activities easier.

One maintenance concern in wet ponds is potential clogging of the pond outlet. Ponds should be designed with a non-clogging outlet such as a reverse-slope pipe, or a weir outlet with a trash rack. A reverse slope pipe draws from below the permanent pool extending in a reverse angle up to the riser and establishes the water elevation of the permanent pool. Because these outlets draw water from below the level of the permanent pool, they are less likely to be clogged by floating debris. Another general rule is that no low flow orifice should be less than 3" in diameter (smaller orifices are more susceptible to clogging).

Direct access is needed to allow maintenance of both the forebay and the main pool of ponds. In addition, ponds should generally have a drain to draw down the pond or forebay to enable periodic sediment clean outs.
Landscaping
Landscaping of wet ponds can make them an asset to a community, and can also enhance the pollutant removal. A vegetated buffer should be created around the pond to protect the banks from erosion, and provide some pollutant removal before runoff enters the pond by overland flow. In addition, ponds should incorporate an aquatic bench (a shallow shelf with wetland plants) around the edge of the pond. This feature provides some pollutant uptake, and also helps to stabilize the soil at the edge of the pond and enhance habitat and aesthetic value.

Design Variations
There are several variations of the wet pond design. Some of these design alternatives are intended to make the practice adaptable to various sites and to account for regional constraints and opportunities.

Wet Extended Detention Pond

The Wet Extended Detention Pond combines the treatment concepts of the dry extended detention pond (for more information see Dry Extended Detention Pond Fact Sheet) and the wet pond (see Figure 2). In this design, the water quality volume is split between the permanent pool and detention storage provided above the permanent pool. During storm events, water is detained above the permanent pool and released over 12 to 48 hours. This design has similar pollutant removal to a traditional wet pond, and consumes less space. Wet Extended Detention Ponds should be designed to maintain at least half the treatment volume in the permanent pool. In addition, designers need to carefully select vegetation planted in the extended detention zone to ensure that it can withstand both wet and dry periods.

Pocket Pond
In this design variation, a pond drains a smaller area than a traditional wet pond, and the permanent pool is maintained by intercepting the groundwater. While this design variation achieves less pollutant removal than a traditional wet pond, it may be an acceptable alternative on sites where space is at a premium, or in a retrofit situation.

Water Reuse Pond
Some designers have used wet ponds to act as a water source, usually for irrigation. In this case, the water balance should account for the water that will be taken from the pond. One study conducted in Florida estimated that a water reuse pond could provide irrigation for a 100-acre golf course at about one seventh the cost of the market rate of the equivalent amount of water ($40,000 versus $300,000).

Regional Adaptations

Semi-Arid Climates
In arid climates, wet ponds are not a feasible option (see Application), but they may be possible in semi-arid climates if the permanent pool is maintained with a supplemental water source, or if the pool is allowed to vary seasonally. This choice needs to be seriously evaluated, however. Saunders and Gilroy (1997) reported that 2.6 acre-feet per year of supplemental water were needed to maintain a permanent pool of only 0.29 acre-feet in Austin, TX (for more information see Stormwater Strategies for Arid and Semiarid Watersheds, Article 66 in The Practice of Watershed Protection).

Cold Climates
Cold climates present many challenges to designers of wet ponds. The spring snowmelt may have a high pollutant load, and large volume to be treated. In addition, cold winters may cause freezing of the permanent pool or freezing at inlets and outlets. Also, high salt concentrations in runoff resulting from road salting may impact pond vegetation, and sediment loads from road sanding may quickly reduce pond capacity.

One means of effectively dealing with spring snowmelt is to use a seasonally operated pond to capture extra snowmelt during the spring, but retain a smaller permanent pool during warmer seasons. In this option, proposed by Oberts (1994), a wet pond has two water quality outlets, both equipped with gate valves. In the summer, the lower outlet is closed. During the fall and throughout the winter, the lower outlet is opened to draw down the permanent pool. As the spring melt begins, the lower outlet is closed to provide detention for the melt event. This method can act as a substitute to using a minimum extended detention storage volume. When wetlands preservation is a downstream objective, seasonal manipulation of pond levels may not be desired (for more information, see Performance of Stormwater Ponds and Wetlands in Winter, Article 71 in The Practice of Watershed Protection). An analysis of the effects on downstream hydrology should be conducted before considering this option. In addition, the manipulation of this system requires some labor and vigilance; a careful maintenance agreement should be confirmed.

Several other modifications help to improve the performance of ponds in cold climates. Designers should consider planting the aquatic buffer with salt-tolerant vegetation if the pond receives road runoff. In order to counteract the effects of freezing on inlet and outlet structures, weirs and larger diameter pipes that are resistant to frost can be used. Designing ponds on-line, which create a continuous flow of water through the pond, also helps prevent freezing of outlet structures. Finally, since freezing of the permanent pool can reduce the effectiveness of pond systems, it may be useful to incorporate extended detention into the design to retain usable treatment area above the permanent pool while it is frozen (for more information, see Performance of Stormwater Ponds and Wetlands in Winter, Article 71 in The Practice of Watershed Protection).

Karst Topography
In karst (i.e., limestone) topography, wet ponds should be designed with an impermeable liner to prevent groundwater contamination or sinkhole formation, and to help maintain the permanent pool.

DEM - Digital Elevation Model

A digital elevation model (DEM) is a digital representation of ground surface topography or terrain. It is also widely known as a digital terrain model (DTM). A DEM can be represented as a raster (a grid of squares) or as a triangular irregular network. DEMs are commonly built using remote sensing techniques, however, they may also be built from land surveying. DEMs are used often in geographic information systems, and are the most common basis for digitally-produced relief maps.
Production

Digital elevation models may be prepared in a number of ways, but they are frequently obtained by remote sensing rather than direct survey. One powerful technique for generating digital elevation models is interferometric synthetic aperture radar; two passes of a radar satellite (such as RADARSAT-1) suffice to generate a digital elevation map tens of kilometers on a side with a resolution of around ten meters. One also obtains an image of the surface cover.

Another powerful technique for generating a Digital Elevation Model is using the digital image correlation method. It implies two optical images acquired with different angles taken from the same pass of an airplane or an Earth Observation Satellite (such as the HRS instrument of SPOT5).

Older methods of generating DEMs often involve interpolating digital contour maps that may have been produced by direct survey of the land surface; this method is still used in mountain areas, where interferometry is not always satisfactory. Note that the contour line data or any other sampled elevation datasets (by GPS or ground survey) are not DEMs, but may be considered digital terrain models. A DEM implies that elevation is available continuously at each location in the study area.

The quality of a DEM is a measure of how accurate elevation is at each pixel (absolute accuracy) and how accurately is the morphology presented (relative accuracy). Several factors play an important role for quality of DEM-derived products:
  • terrain roughness;
  • sampling density (elevation data collection method);
  • grid resolution or pixel size;
  • interpolation algorithm;
  • vertical resolution;
  • terrain analysis algorithm;

Stormwater Software - RMA 2

RMA2 is a hydrodynamic modeling code that supports subcritical flow analysis, including wetting and drying and marsh porosity models. It is part of the TABS analysis package written by the U.S. Army Corps of Engineers Waterways Experiment Station (USACE-WES). The methods of analysis used by the TABS codes along with their file formats and input parameters are described in their own documents. SMS supports both pre- and post-processing for RMA2.A mesh for use with RMA2 is created and edited in SMS using the Mesh Module. The modeling parameters required by RMA2 are generated and applied to the mesh using commands grouped in the RMA2 menu. Post processing of solution data generated by RMA2 is done using the generic visualization tools of SMS

Stormwater Software - MUSIC

Taken from http://www.ecosol.com.au/music.asp


MUSIC Stormwater Management System

Introduction to MUSIC

MUSIC is an acronym for Modelling Software for Urban Stormwater Improvement Conceptualisation. It is a product of the Cooperative Research Centre for Catchment Hydrology (now eWater CRC) and the licensor is Monash University.

MUSIC provides a user-friendly decision support system that enables planners to evaluate conceptual designs of stormwater management systems to meet water quality objectives for their catchment and requirements with respect to water-sensitive urban design.

MUSIC allows complex stormwater management scenarios to be quickly and efficiently created and the results to be viewed using a range of graphical and tabular formats. This reduces the uncertainty surrounding the planning of stormwater management strategies, and may generate substantial cost-savings.

To use MUSIC you need to register and pay a fee (currently $330) to download the software. Training and support is provided by the eWater CRC.
Purpose
MUSIC is designed to simulate urban stormwater systems operating at a range of temporal and spatial scales for catchments from 0.01km2 to 100km2 and modelling time steps ranging from 6 minutes to 24 hours to match the catchment scale.
Target user
MUSIC is designed for urban stormwater engineers, planners, policy staff, consultants as well as state, regional, and local government authorities. An understanding of stormwater management principles and practices is required to use MUSIC.
Application of MUSIC to modelling GPTs

Double clicking a GPT icon within MUSIC produces a popup window that requires the following data to be input:
1. low flow bypass;
2. high flow bypass; and
3. piecewise-linear user-definable transfer functions for the GPT performance in capturing Gross Pollutants (GP), Total Suspended Solids (TSS), Total Phosphorus (TP), and Total Nitrogen (TN). In each case the independent variable is input concentration (mg/l or kg/MI) and the dependent variable is the output concentration.
The GPT inputs are independent of the flow rate, except that there are underflow and overflow limits. Flow below the underflow limit, and flow above the overflow limit, passes through with no change of concentration.
Important consideration for MUSIC user
The validity of the predictions is only as good as the validity of the input data. All GPT performance predictions are subject to uncertainty owing to the stochastic nature of environmental processes, with quantities varying chaotically with time and location. The difficulty in making repeatable measurements is illustrated in the wide range of published test results. This is not surprising considering that there can be significant differences, for example in the:
  • catchment type and hydrology;
  • weather conditions and events during the testing period;
  • sampling regimes – frequency, timing, and location;
  • composition of pollutant load;
  • nutrient transport mechanisms;
  • level of bonding of nutrients to suspended solids
  • degradation of accumulated pollutants;
  • suspended solid particle size distribution (PSD); and the size and state of the unit (i.e. how well it has been cleaned and maintained).

Consequently, when comparing different GPTs, it is important to understand that the results may have been derived in conditions that vary significantly. There is no industry-wide standard for determining the input values required by MUSIC.

Capture Efficiency of Nutriens (TP and TN)

GPTs capture are designed primarily to capture solid particles but, because they attach to these particles, nutrients are also captured. This is measured in terms of TSS capture efficiency. It follows then that GPTs with the same TSS performance will remove the same level of nutrients as along as all other conditions are the same.

The most comprehensive measurement of GPT nutrient capture in Australia was reported in Walker et. al. 1991, a document referenced in Appendix C3 of the MUSIC development team, CRC for Catchment Hydrology (revised February 2005 for MUSIC v2.1). This documents quotes “approximately 30%” TP removal and also found that although TN removal was erratic during storm events, there was “consistent removal of approximately 13% of TN during dry weather flow conditions”.


The MUSIC input data must be viewed as an overall long-term average – in the short term there are simply too many fluctuations making any conclusions largely meaningless. The long-term pollutant capture performance depends not only on the make and type of GPT but how it is managed and maintained.


If inappropriate pollutant removal practices are used to clean the GPT (such as clamshell or removable basket, where much of the sediment is returned to the unit through draining and then subsequently remobilised), it is obvious that claimed nutrient removal rates will be reduced significantly. This is one of the most significant benefits from using the vacuum method, which ensures that all pollutants are removed form the unit.


Recommendations for MUSIC input values for Ecosol units are provided at the bottom of each product page. Click for RSF 100, RSF 1000 and RSF 4000.

Stormwater Software - 12D

Taken from http://www.12d.com/

Established in 1988, 12D Solutions sells and supports its principal product suite, 12d Model (formerly known as 4d Model) direct and through distributors around the world.

12D Solutions clients include civil and water engineering consultants; environmental consultants; surveyors; local; state and national government departments and authorities; research institutes; construction companies and mining consultants.

12d Model is a powerful terrain modelling, surveying and civil engineering software package. It allows fast production in a wide variety of projects including roads, rail, site layouts, and environmental impact studies.

12d Model is a powerful terrain modelling, surveying and civil engineering package. It allows fast production in a wide variety of projects including roads, site layouts, subdivisions and Environmental Impact studies.

Using 12d Models screen menus and fast interactive graphics, the user effortlessly moves through a design.
With 12d Models powerful design capabilities, difficult surveying and civil design tasks can be easily visualized and completed.
Projects such as roads, channels, storage tanks, subdivisions, landscaping, rail studies, major pipelines, waste water reticulation and general site works are efficiently handled with 12d Model.
12d Model includes a powerful programming language which allows users to build their own options from 12d Models extensive programming library.
12d Model features data exchange with drainage and river analysis packages including XP-SWMM, XP-UDD, Drains, ILSAX, PC Drain, RATHGL and HEC-RAS, survey packages such as TP Setout as well as the CAD systems IntelliCAD, AutoCAD and Microstation.
12d Model is a totally Australian product, running on Windows NT, 95, 98, 2000 and XP (including PC Notebooks).
12d Model has been specifically designed for easy use. It is ideal for use at all stages of projects, and is particularly useful for large route selection and corridor studies.12d Model is an essential tool in today's fiercely competitive business climate.
Rivers
There are six modules for rivers work: HEC RAS Advanced, XP SWMM, Mike 11, UNET and ISIS.
These modules create the natural cross section files for HEC RAS, XP-SWMM, XP-UDD, Mike11, UNET and ISIS respectively. The water level results from these packages can then be read back into 12d to create a detailed water surface that accurately defines the river bank between the defined cross sections. This water surface is used to create 3d images, movie files of flight or walks down the river, cross section plots. river profiles and plan drawings coloured and contoured by depth.
Historical flood data can also be presented in 12d Model using the "river mapper". This interface creates a water surfaces from existing water level data. The interface uses "shape strings" to add incredible power and flexibility to the mapping process. Meandering streams and off line storages can easily be mapped without burdening your hydraulic modelling package with additional cross section calculations.
The 12d Model Rivers modules read numerous data formats including HEC2 data, EEBY cross section data, USGS DEM formats and xyz data. The add on AutoCAD DWG/DXF and Microstation DGN modules enable existing drawing/elevation data to be imported to 12d.
Elevation data can be combined from several sources and manipulated to form a final ground surface from which cross section data is created.
The modules generate cross sections, measure channel and overbank distances, mark left and right bank locations and automatically mark levee locations for HEC RAS. User specified steady state discharges and Manning's "n" values are exported as initial starting values.
Raster georeferenced images (which can exceed one gigabyte in size) can be used as backdrops for defining your river bank locations. For simple projects, channel improvements are easily designed and volumes calculated using 12d Model Base. Complex designs and volumes may require other modules.
The Rivers modules are:
HEC RAS Advanced, XP SWMM & MIKE 11

These river interface modules work on branched river systems. The complete project is created for the river design programs and for unsteady flow conditions. The maximum water levels are read back into 12d Model.

UNET
In addition to cross section data, this module also exports reservoir storage areas.

ISIS
ISIS has the most comprehensive interface of the Rivers modules. Volumes for online and offline reservoirs are exported and cross sections are created for spill sections as well as river cross sections.
Urban Drainage

The Drainage module allows the design of drainage networks, typically those required for new land subdivisions and development projects.
The drainage string itself consists of manholes, joined by straight or curved pipes. Invert levels and pipe grades can be set or modified graphically or by typed input. Manhole and pipe sizes are also user definable.
Drainage design can be as simple or complex as the project dictates. 12d automatically determines pipe grade based on minimum slope and cover while services clashes are displayed graphically. Data is exported to the design packages Drains, PCdrain, XP-SWMM, XP-UDD, RAT2000, RATHGL, ILSAX, WINDES (Micro Drainage) and spreadsheets. The data exported can be as simple as catchment areas or as advanced as pit inlet capacity and overland flow (determined inside 12d by measuring road cross fall and grade). Even maximum ponding levels and volumes can be determined for inlet in SAG inlet conditions.
Results from the design packages can be read back into 12d enabling the user to....
  • update 12d with the new inverts and pipe sizes from the drainage design software.
  • plot customised drainage long sections with service crossings, hydraulic grade line, flow, velocity and/or user defined data. Services that cross the drainage pipe and those within a user defined corridor (parallel to the pipe) are also included.
  • plot customised plan drawings indicating catchments, pipe sizes and types, inverts and more.
  • print pit construction schedules in predefined or custom formats.
  • produce pit/pipe quantity schedules by pipe sizes, depths, types etc (all custom defined).
    detailed excavation volumes reflecting pipe sizes, over excavation for bedding materials and user defined trench shapes. Volumes by depth can then be calculated using the 12d volumes package.
  • calculate and display/plot flooded areas from overflow volumes or overland flow discharges (normal depth calculations).
  • create HEC RAS project files for detailed backwater calculations in critical areas.

Sewer - Waste Water Reticulation


The Sewer module is an extension of the Drainage module and supports the design of gravity operated waste water reticulation systems, typically those required for new land subdivisions (estates) and development projects.

The user enters proposed manholes, pipelines and end of line points. Obstructions which pass over, under or parallel to the design lines within a user specified corridor about the design line will be shown on long and cross section views.

When satisfied with the design invert levels, connections from the design line to the individual house blocks can be added and reported on.Earthwork volumes for trenches can be calculated along the selected design line.

The special waste water reticulation longitudinal plots show existing surface, manholes, design pipelines, pipe grades, property connection points and all obstructions. Long section plots to the Melbourne Water standard are included.

Pipeline


This module is used to support the design of major pipelines of any diameter (for example, 2000 mm) and any length.


The module allows for the extraction of long sections and cross sections against the digital terrain model for the proposed route, plus all the obstructions that run parallel to or cross a corridor of user given width on either side of the centre line of the route.


The joint deflection for pipes of a user nominated length is calculated and interactively displayed along the pipeline.


Earthwork volumes for trenches can be calculated along the selected design line.


The special pipeline longitudinal plots show the existing surface, design pipeline, depth of cut or fill to pipe invert, percentage grades and vertical curve data or deflection angles, and all obstructions.

Stormwater Software - HEC-HMS

Taken from http://www.hec.usace.army.mil/software/hec-hms/




The Hydrologic Modeling System (HEC-HMS) is designed to simulate the precipitation-runoff processes of dendritic watershed systems. It is designed to be applicable in a wide range of geographic areas for solving the widest possible range of problems. This includes large river basin water supply and flood hydrology, and small urban or natural watershed runoff. Hydrographs produced by the program are used directly or in conjunction with other software for studies of water availability, urban drainage, flow forecasting, future urbanization impact, reservoir spillway design, flood damage reduction, floodplain regulation, and systems operation.

The program is a generalized modeling system capable of representing many different watersheds. A model of the watershed is constructed by separating the hydrologic cycle into manageable pieces and constructing boundaries around the watershed of interest. Any mass or energy flux in the cycle can then be represented with a mathematical model. In most cases, several model choices are available for representing each flux. Each mathematical model included in the program is suitable in different environments and under different conditions. Making the correct choice requires knowledge of the watershed, the goals of the hydrologic study, and engineering judgment.

The program features a completely integrated work environment including a database, data entry utilities, computation engine, and results reporting tools. A graphical user interface allows the seamless movement between the different parts of the program. Program functionality and appearance are the same across all supported platforms.

Contents:

Watershed Physical Description

The physical representation of a watershed is accomplished with a basin model. Hydrologic elements are connected in a dendritic network to simulate runoff processes. Available elements are: subbasin, reach, junction, reservoir, diversion, source, and sink. Computation proceeds from upstream elements in a downstream direction.

An assortment of different methods is available to simulate infiltration losses. Options for event modeling include initial constant, SCS curve number, gridded SCS curve number, exponential, and Green Ampt. The one-layer deficit constant method can be used for simple continuous modeling. The five-layer soil moisture accounting method can be used for continuous modeling of complex infiltration and evapotranspiration environments. Gridded methods are available for both the deficit constant and soil moisture accounting methods.

Several methods are included for transforming excess precipitation into surface runoff. Unit hydrograph methods include the Clark, Snyder, and SCS techniques. User-specified unit hydrograph or s-graph ordinates can also be used. The modified Clark method, ModClark, is a linear quasi-distributed unit hydrograph method that can be used with gridded meteorologic data. An implementation of the kinematic wave method with multiple planes and channels is also included.

Multiple methods are included for representing baseflow contributions to subbasin outflow. The recession method gives an exponentially decreasing baseflow from a single event or multiple sequential events. The constant monthly method can work well for continuous simulation. The linear reservoir method conserves mass by routing infiltrated precipitation to the channel.

A variety of hydrologic routing methods are included for simulating flow in open channels. Routing with no attenuation can be modeled with the lag method. The traditional Muskingum method is included along with the straddle stagger method for simple approximations of attenuation. The modified Puls method can be used to model a reach as a series of cascading, level pools with a user-specified storage-discharge relationship. Channels with trapezoidal, rectangular, triangular, or circular cross sections can be modeled with the kinematic wave or Muskingum-Cunge methods. Channels with overbank areas can be modeled with the Muskingum-Cunge method and an 8-point cross section.

Water impoundments can also be represented. Lakes are usually described by a user-entered storage-discharge relationship. Reservoirs can be simulated by describing the physical spillway and outlet structures. Pumps can also be included as necessary to simulate interior flood area. Control of the pumps can be linked to water depth in the collection pond and, optionally, the stage in the main channel.

Meteorology Description

Meteorologic data analysis is performed by the meteorologic model and includes precipitation, evapotranspiration, and snowmelt. Six different historical and synthetic precipitation methods are included. Two evapotranspiration methods are included at this time. Currently, only one snowmelt method is available.

Four different methods for analyzing historical precipitation are included. The user-specified hyetograph method is for precipitation data analyzed outside the program. The gage weights method uses an unlimited number of recording and non-recording gages. The Thiessen technique is one possibility for determining the weights. The inverse distance method addresses dynamic data problems. An unlimited number of recording and non-recording gages can be used to automatically proceed when missing data is encountered. The gridded precipitation method uses radar rainfall data.

Four different methods for producing synthetic precipitation are included. The frequency storm method uses statistical data to produce balanced storms with a specific exceedance probability. Sources of supporting statistical data include Technical Paper 40 and NOAA Atlas 2. While it was not specifically designed to do so, data can also be used from NOAA Atlas 14. The standard project storm method implements the regulations for precipitation when estimating the standard project flood. The SCS hypothetical storm method implements the primary precipitation distributions for design analysis using Natural Resources Conservation Service (NRCS) criteria. The user-specified hyetograph method can be used with a synthetic hyetograph resulting from analysis outside the program.

Potential evapotranspiration can be computed using monthly average values. There is also an implementation of the Priestley-Taylor method that includes a crop coefficient. A gridded version of the Priestley-Taylor method is also available.

Snowmelt can be included for tracking the accumulation and melt of a snowpack. A temperature index method is used that dynamically computes the melt rate based on current atmospheric conditions and past conditions in the snowpack.

Hydrologic Simulation

The time span of a simulation is controlled by control specifications. Control specifications include a starting date and time, ending date and time, and a time interval.

A simulation run is created by combining a basin model, meteorologic model, and control specifications. Run options include a precipitation or flow ratio, capability to save all basin state information at a point in time, and ability to begin a simulation run from previously saved state information.

Simulation results can be viewed from the basin map. Global and element summary tables include information on peak flow and total volume. A time-series table and graph are available for elements. Results from multiple elements and multiple simulation runs can also be viewed. All graphs and tables can be printed.

Parameter Estimation

Most parameters for methods included in subbasin and reach elements can be estimated automatically using optimization trials. Observed discharge must be available for at least one element before optimization can begin. Parameters at any element upstream of the observed flow location can be estimated. Six different objective functions are available to estimate the goodness-of-fit between the computed results and observed discharge. Two different search methods can be used to minimize the objective function. Constraints can be imposed to restrict the parameter space of the search method.

Analyzing Simulations

Analysis tools are designed to work with simulation runs to provide additional information or processing. Currently, the only tool is the depth-area analysis tool. It works with simulation runs that have a meteorologic model using the frequency storm method. Given a selection of elements, the tool automatically adjusts the storm area and generates peak flows represented by the correct storm areas.

GIS Connection

The power and speed of the program make it possible to represent watersheds with hundreds of hydrologic elements. Traditionally, these elements would be identified by inspecting a topographic map and manually identifying drainage boundaries. While this method is effective, it is prohibitively time consuming when the watershed will be represented with many elements. A geographic information system (GIS) can use elevation data and geometric algorithms to perform the same task much more quickly. A GIS companion product has been developed to aid in the creation of basin models for such projects. It is called the Geospatial Hydrologic Modeling Extension (HEC-GeoHMS) and can be used to create basin and meteorologic models for use with the program.

Stormwater Software - HEC-RAS

Taken from http://www.hec.usace.army.mil/software/hec-ras/




HEC-RAS allows you to perform one-dimensional steady flow, unsteady flow, sediment transport/mobile bed computations, and water temperature modeling.HEC-RAS is designed to perform one-dimensional hydraulic calculations for a full network of natural and constructed channels. The following is a description of the major capabilities of HEC-RAS.

1. User interface
2. Hydraulic Analysis Components
3. Data Storage and Management
4. Graphics and Reporting.




User Interface

The user interacts with HEC-RAS through a graphical user interface (GUI). The main focus in the design of the interface was to make it easy to use the software, while still maintaining a high level of efficiency for the user. The interface provides for the following functions:

  • File Management
  • Data Entry and Editing
  • Hydraulic Analyses
  • Tabulation and Graphical Displays of Input and Output Data
  • Reporting Facilities
  • Context Sensitive Help

Hydraulic Analysis Components

The HEC-RAS system contains four one-dimensional river analysis components for: (1) steady flow water surface profile computations; (2) unsteady flow simulation; (3) movable boundary sediment transport computations; and (4) water quality analysis. A key element is that all four components use a common geometric data representation and common geometric and hydraulic computation routines. In addition to the four river analysis components, the system contains several hydraulic design features that can be invoked once the basic water surface profiles are computed.


Steady Flow Water Surface Profiles.

This component of the modeling system is intended for calculating water surface profiles for steady gradually varied flow. The system can handle a full network of channels, a dendritic system, or a single river reach. The steady flow component is capable of modeling subcritical, supercritical, and mixed flow regimes water surface profiles.
The basic computational procedure is based on the solution of the one-dimensional energy equation. Energy losses are evaluated by friction (Manning’s equation) and contraction/expansion (coefficient multiplied by the change in velocity head). The momentum equation may be used in situations where the water surface profile is rapidly varied. These situations include mixed flow regime calculations (i.e. hydraulic jumps), hydraulics of bridges, and evaluating profiles at river confluences (stream junctions).

The effects of various obstructions such as bridges, culverts, weirs, and structures in the flood plain may be considered in the computations. The steady flow system is designed for application in flood plain management and flood insurance studies to evaluate floodway encroachments. Also, capabilities are available for assessing the change in water surface profiles due to channel improvements, and levees. Special features of the steady flow component include: multiple plan analyses; multiple profile computations; multiple bridge and/or culvert opening analyses; and split flow optimization.

Unsteady Flow Simulation.


                  Unsteady Flow Simulation. This component of the HEC-RAS modeling system is capable of simulating one-dimensional unsteady flow through a full network of open channels. The unsteady flow equation solver was adapted from Dr. Robert L. Barkau's UNET model (Barkau, 1992 and HEC, 1997). The unsteady flow component was developed primarily for subcritical flow regime calculations. However, with the release of Version 3.1, the model can now performed mixed flow regime (subcritical, supercritical, hydraulic jumps, and draw downs) calculations in the unsteady flow computations module.

                  The hydraulic calculations for cross-sections, bridges, culverts, and other hydraulic structures that were developed for the steady flow component were incorporated into the unsteady flow module.Special features of the unsteady flow component include: Dam break analysis; levee breaching and overtopping; Pumping stations; navigation dam operations; and pressurized pipe systems.

                  Sediment Transport/Movable Boundary Computations

                  This component of the modeling system is intended for the simulation of one-dimensional sediment transport/movable boundary calculations resulting from scour and deposition over moderate time periods (typically years, although applications to single flood events are possible).

                  The sediment transport potential is computed by grain size fraction, thereby allowing the simulation of hydraulic sorting and armoring. Major features include the ability to model a full network of streams, channel dredging, various levee and encroachment alternatives, and the use of several different equations for the computation of sediment transport.

                  The model is designed to simulate long-term trends of scour and deposition in a stream channel that might result from modifying the frequency and duration of the water discharge and stage, or modifying the channel geometry. This system can be used to evaluate deposition in reservoirs, design channel contractions required to maintain navigation depths, predict the influence of dredging on the rate of deposition, estimate maximum possible scour during large flood events, and evaluate sedimentation in fixed channels.

                  Water Quality Analysis


                This component of the modeling system is intended to allow the user to perform riverine water quality analyses. An advection-dispersion module is included with this version of HEC–RAS, adding the capability to model water temperature. This new module uses the QUICKEST-ULTIMATE explicit numerical scheme to solve the one-dimensional advection-dispersion equation using a control volume approach with a fully implemented heat energy budget. Transport and Fate of a limited set of water quality constituents is now also available in HEC-RAS. The currently available water quality constituents are: Dissolved Nitrogen (NO3-N, NO2-N, NH4-N, and Org-N); Dissolved Phosphorus (PO4-P and Org-P); Algae; Dissolved Oxygen (DO); and Carbonaceous Biological Oxygen Demand (CBOD).

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