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DOI | 10.1029/2018WR023297 |
A Dynamic Multidomain Green-Ampt Infiltration Model | |
Stewart, Ryan D. | |
2018-09-01 | |
发表期刊 | WATER RESOURCES RESEARCH |
ISSN | 0043-1397 |
EISSN | 1944-7973 |
出版年 | 2018 |
卷号 | 54期号:9页码:6844-6859 |
文章类型 | Article |
语种 | 英语 |
国家 | USA |
英文摘要 | Shrink-swell soils possess dynamic hydraulic properties, which may limit the applicability of traditional models for simulating infiltration and overland flow. This study incorporates Green-Ampt infiltration concepts into a multidomain porosity framework to account for variations in pore size distributions and saturated hydraulic conductivities caused by soil shrinkage and swelling. The model requires three input variables (initial water content, rainfall rate, and time) and up to 15 parameters to simulate infiltration and overland flow, though most of the parameters are universal constants or can be estimated from auxiliary measurements. In comparison, the classic Green-Ampt model, which assumes constant hydraulic properties and a single domain, requires the same three inputs and up to seven parameters to use. Performance of the proposed multidomain model was verified with two data sets. The first came from a study in Mexico where time to ponding and soil matrix infiltration were quantified under simulated rainfall, and the second came from a study in Chile where overland flow was measured during irrigation experiments on runoff plots. By tuning two (Chile) or three (Mexico) parameters, the multidomain model provided accurate estimations of infiltration/runoff partitioning at multiple scales. Compared to the classic single-domain model, the multidomain model had lower root-mean-square deviations (reducing simulated infiltration errors by 2-3 times) and Akaike Information Criterion (AIC) scores (Delta AIC similar to 100), thus providing better simulations of infiltration, ponding, and runoff. These results demonstrate that modeling hydrological processes in shrink-swell soils necessitates separating soil properties mediated by the matrix from those associated with interblock shrinkage cracks. Plain Language Summary Many soils develop cracks as they dry. During rainstorms and irrigation events, these cracks permit water to move rapidly, but we do not currently possess appropriate tools to simulate water movement in such conditions. This study proposes a mathematical model that calculates water infiltration into such soils by explicitly accounting for properties of cracks versus those of the surrounding soil. The model was verified using field observations from two locations, which demonstrated that the model can accurately simulate water infiltration, ponding on the soil surface, and surface runoff in soils containing cracks. |
英文关键词 | shrink-swell soil vertisols overland flow cracks surface runoff bypass flow |
领域 | 资源环境 |
收录类别 | SCI-E |
WOS记录号 | WOS:000448088100055 |
WOS关键词 | HEAVY CLAY SOIL ; HYDRAULIC CONDUCTIVITY ; PREFERENTIAL FLOW ; SHRINKAGE GEOMETRY ; WATER ; TRANSPORT ; MACROPORES ; CRACKING |
WOS类目 | Environmental Sciences ; Limnology ; Water Resources |
WOS研究方向 | Environmental Sciences & Ecology ; Marine & Freshwater Biology ; Water Resources |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/21370 |
专题 | 资源环境科学 |
作者单位 | Virginia Polytech Inst & State Univ, Sch Plant & Environm Sci, Blacksburg, VA 24061 USA |
推荐引用方式 GB/T 7714 | Stewart, Ryan D.. A Dynamic Multidomain Green-Ampt Infiltration Model[J]. WATER RESOURCES RESEARCH,2018,54(9):6844-6859. |
APA | Stewart, Ryan D..(2018).A Dynamic Multidomain Green-Ampt Infiltration Model.WATER RESOURCES RESEARCH,54(9),6844-6859. |
MLA | Stewart, Ryan D.."A Dynamic Multidomain Green-Ampt Infiltration Model".WATER RESOURCES RESEARCH 54.9(2018):6844-6859. |
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