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Hardy Cross-metoden×MODFLOW Grundvandsmodellering×Muskingum-modellering×
FagområdeByggeteknikByggeteknikByggeteknik
FamilieProcess / pipelineProcess / pipelineProcess / pipeline
Oprindelsesår19361984 (original release); continuously updated through MODFLOW-6 (2017)1938
OphavspersonHardy CrossMichael G. McDonald and Arlen W. Harbaugh (U.S. Geological Survey)George McCarthy
TypeIterative method for pipe network flow distributionNumerical groundwater flow simulationHydrologic method for flood attenuation in rivers
Oprindelig kildeCross, H. (1936). Analysis of flow in networks of conduits or conductors. University of Illinois Bulletin, 34(17), 3-29. link ↗Harbaugh, A. W. (2005). MODFLOW-2005, the U.S. Geological Survey modular ground-water model — the Ground-Water Flow Process. U.S. Geological Survey Techniques and Methods 6-A16. link ↗McCarthy, G. T. (1938). The Unit Hydrograph and Flood Routing. US Army Corps of Engineers Document 608. link ↗
AliasserCross method, Moment distribution method, Iterative balancingMODFLOW-2005, MODFLOW-6, modular groundwater flow model, USGS groundwater modelFlood routing, Stream flow attenuation, Hydrologic routing
Relaterede303
ResuméThe Hardy Cross method is an iterative technique for solving steady-state flow distribution in pipe networks, originally developed for water distribution systems. Introduced by Hardy Cross in 1936, this method balances flow continuity and pressure head constraints through successive iterations, making it ideal for hand calculations and gaining physical insight into network behavior.MODFLOW is the U.S. Geological Survey's open-source, modular finite-difference model for simulating three-dimensional groundwater flow through porous media. First released in 1984 and continuously updated — most recently as MODFLOW-6 — it is the global standard for quantitative hydrogeological analysis, widely used in civil engineering, environmental consulting, water-resource management, and groundwater contamination studies.The Muskingum method is a hydrologic flood routing technique that predicts how a flood wave attenuates (reduces in peak) and spreads as it travels down a river reach. Developed by McCarthy in 1938 for the US Army Corps of Engineers, the method is simple enough for hand calculations while capturing the essential physics of flood propagation.
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ScholarGateSammenlign metoder: Hardy Cross Method · MODFLOW Groundwater Modeling · Muskingum Routing. Hentet 2026-06-18 fra https://scholargate.app/da/compare