Advanced(°í±Þ ¾Ë°í¸®Áò)
RiverFLO-2D´Â ÷´Ü À¯ÇÑ ¿ä¼Ò ÇØ¹ý ¾Ë°í¸®ÁòÀ» »ç¿ëÇÏ¿© À¯»ç ¸ðÇüµéÀÌ °®´Â ´ëºÎºÐÀÇ ´ÜÁ¡µéÀ» ÇØ°áÇØ ÁÝ´Ï´Ù. ¸í½ÃÀû ½Ã°£-°£°Ý ¾Ë°í¸®ÁòÀº ¹æ´ëÇÑ ¸ÅÆ®¸¯½º ü°èÀÇ ¼Ö·ç¼ÇÀ» ¿ä±¸ÇÏÁö ¾Ê°í, È¿À²Àû º´·ÄÈ¿¡ ´ëÇÑ À¯¿¬¼ºÀ» Á¦°øÇÕ´Ï´Ù.
Stable(¾ÈÁ¤¼º)
RiverFLO-2D´Â ÃÊÀÓ°è ¹× ¹ÌÀÓ°è È帧(Supercritical & Subcritical Flows)¿¡ ´ëÇØ ¸Å¿ì ºü¸£°í º¸´Ù ¾ÈÁ¤ÀûÀÎ 2Â÷¿ø À¯ÇÑ ¿ä¼Ò ¸ðÇüÀ» Á¦°øÇÕ´Ï´Ù. ÄÄÇ»ÅÍ ÄÚµå´Â OpenMP Ç¥ÁØ ¸í·É¾îµéÀ» »ç¿ëÇÏ°í º´·ÄÈÇÔÀ¸·Î½á ¿¬»ê ½Ã°£À» Å©°Ô ´ÜÃà½ÃÄÑÁÖ°í, MS-Windows XP ¶Ç´Â Vista ¿î¿µÃ¼Á¦¸¦ »ç¿ëÇÏ´Â ´ÙÁßÄÚ¾î ÄÄÇ»ÅÍ(Duo/Quad)ÀÇ ÀÌÁ¡À» ÀÌ¿ëÇÕ´Ï´Ù.
Accurate(Á¤È®¼º)
RiverFLO-2D´Â Mass conservative & Robust Dry-Wet treatment method¸¦ Á¦°øÇÏ¿© ÀÎÀ§ÀûÀÎ ¼Óµµ(Velocities)³ª ¼Â¡(Surging)À» ¸¸µéÁö ¾Ê°í Å« ¸Þ½Ã(mesh) ¿µ¿ªÀ» °ÇÁ¶(dry)ÇÒ ¼ö ÀÖ½À´Ï´Ù. ÀÌ ¸ðÇüÀº ½Ã¹Ä·¹ÀÌ¼Ç ÁøÇàÀ» ÅëÇØ ¸ðÇüÀÇ Á¤È®¼ºÀ» Æò°¡ÇÔ°ú ¾Æ¿ï·¯ üÀû º¸Á¸(Volume Conservation)¿¡ °üÇØ ¸®Æ÷Æ®ÇØ ÁÝ´Ï´Ù.
Productive(»ý»ê¼º)
RiverFLO-2D´Â ¸ðÇü ¼³Á¤¿¡ ¼Ò¿ä µÇ´Â ½Ã°£À» ÃÖ¼ÒÈÇÒ ¼ö ÀÖ¾î º¸´Ù ¸¹Àº ½Ã³ª¸®¿À¸¦ ½ÇÇàÇØ º¼ ¼ö ÀÖ°í ½ÇÁ¦ ¸ðÇü ÀÀ¿ë°ú °á°ú ºÐ¼®¿¡ ÁýÁßÇÒ ¼ö ÀÖ½À´Ï´Ù. RiverFLO-2D´Â ° ¹Ù´Ú Àüü°¡ °ÇÁ¶ÇÏ´õ¶óµµ ½ÇÁ¦ Ãʱ⠻óŸ¦ °®°í ½Ã¹Ä·¹À̼ÇÀ» ÇÒ ¼ö ÀÖÀ¸¹Ç·Î º¸´Ù »ý»ê¼ºÀ» ³ôÀ̵µ·Ï µµ¿ÍÁÝ´Ï´Ù.
RiverFlo-2D »ç¿ëÀÚ ÀÎÅÍÆäÀ̽º´Â Argus Open ¼öÄ¡ ȯ°æ(Argus ONE)¿¡ ±âÃʸ¦ µÐ, GIS ÅëÇÕ ¼ÒÇÁÆ®¿þ¾î ü°è·Î À¯ÇÑ ¿ä¼Ò ¸Þ½Ã(mesh)¸¦ ¸¸µé°í ´Ùµë±â À§ÇÑ ÀÎÅÍ·¢Æ¼ºê ÇÔ¼öµéÀ» Á¦°øÇÕ´Ï´Ù. ¶ÇÇÑ, °æ°è Á¶°ÇÀ» ½±°Ô ÇÒ´çÇÒ ¼ö ÀÖ°Ô ÇØÁÝ´Ï´Ù.
Model Applications
RiverFLO-2D¸¦ °íÁ¤ ¹Ù´Ú(Rigid bed) ¶Ç´Â À̵¿ ¹Ù´Ú(mobile bed) Ȱ¿ë¿¡ ´ëÇØ ½Ã°£ Á¾¼Ó ¹× ¾ÈÁ¤ »óÅÂ(Steady-State)ÀÇ 2Â÷¿ø ÇÏõ ½Ã¹Ä·¹À̼ǿ¡ Àû¿ëÇÒ ¼ö ÀÖ½À´Ï´Ù. ÀÌ ¸ðÇüÀº À¯µ¿Àå(flow field)À» »ó¼¼È÷ ¹¦»çÇÏ´Â °íÇØ»óµµÀÇ °ø°£Àû º¯¼ö °á°ú¸¦ »ý¼ºÇÕ´Ï´Ù. º» ¸ðÇüÀº ÀϹÝÀûÀ¸·Î ¾Æ·¡¿Í °°Àº ºÐ¾ß¿¡ Àû¿ëÇÒ ¼ö ÀÖ½À´Ï´Ù.
Detailed in-channel river hydrodynamics
ÇÏõ Á¦¹æ ¹ü¶÷(River overbank flooding)
Á¦¹æ Á¦°Å(Levee removal)
´ï-ºØ±« È«¼ö ºÐ¼®(Dam-break flood analysis)
Åä»ç À̵¿ ? À̵¿ ¹Ù´Ú(Sediment transport - mobile bed)
Á¦¹æ ħ½Ä ¹æÁö ¼³°è ¹× ºÐ¼®(Bank erosion protection design and analysis)
° º¹¿ø ¼³°è(River restoration design)
 |
 |
| A.S.A.P. Modeling with RiverFLO-2D |
¹Ì±¹ ¿ö½ÌÅÏ Hoh °ÀÇ Á¦¹æ º¸È£ ÇÁ·ÎÁ§Æ®¿¡¼ ¼³°èµÈ
Log Jams ÁÖº¯ÀÇ »ó¼¼ À¯ÇÑ ¿ä¼Ò ¸Þ½Ã |
Model Formulation(¸ðÇü ü°è)
¹æÁ¤½Ä RiverFLO-2D is based on the depth-averaged equations that govern free surface flow, sediment transport and bed evolution in rivers:
With the sediment transport module, users can select from six sediment transport capacity formulas for mobile bed applications, including, Meyer-Peter and Muller, Yang, Ackers-White, Karim-Kennedy, Toffaleti, and Wilcock-Crowe for gravel-bed rivers. Bed aggradation and degradation is tracked. As an example, RiverFLO-2D procedure based on the Meyer-Peter and Muller formulation uses the following equations:
Solution method
The Finite Element Method is the preferred numerical approach for detailed in-channel river analysis because the finite element mesh adapts to irregular channel geometry. The method is also supported by a solid mathematical foundation. RiverFLO-2D implements an efficient four-step explicit time-stepping scheme to solve the full dynamic wave momentum equations. RiverFLO-2D does not require adding artificial diffusion to stabilize the numerical solution. The spatial discretization uses triangular elements and since the solution method is explicit, it does not involve solution of large matrix systems. RiverFLO-2D has a robust mass (volume) conservative drying-wetting algorithm that permits portions of the mesh to become repetitively dry and wet during simulations. Some 2D channel models cannot simulate an initial dry river bed, and require a time-consuming mesh draining process until the actual dry bed conditions are reached. This is commonly known as model spin-down. In RiverFLO-2D, the river bed may be initially dry or it may become dry during the simulation and the model does not require the costly spin-down computational process.
Parallelization for multiple processor computers
RiverFLO-2D parallelized computer code, takes advantage of multi-core computers that use MS-Windows XP or Vista operating systems. Most 2D hydraulic models are either based on sequential codes that do not utilize multiple-threading programming techniques or have been parallelized in computer cluster environments that are often not accessible to many consulting engineering companies and government agencies. Tests in multi-core processor computers indicate that the RiverFLO-2D model is able to run up to 2.5 faster than the sequential code in single processor computers.
Verification
To verify RiverFLO-2D capabilities to simulate river hydrodynamics, the model has been tested following the procedures recommended by the ASCE 3D Flow Model Verification and Validation Committee. This validation process involved testing the model with analytical solutions and simplified cases, comparison against laboratory experiments and application to field scale projects with available data. RiverFLO-2D testing results have been published in peer-reviewed journals. Application to field scale problems, such as the well-known Malpasset dam-break event, reveals that the model accurately replicates wave travel times and measured water surface elevations on an initially dry river bed.

|