Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.proenv.2013.06.071 |
Consequences of salinity-induced-time-dependent soil hydraulic properties on flow and transport in salt-affected soils | |
Russo, David | |
通讯作者 | Russo, David |
会议名称 | International Conference on Four Decades of Progress in Monitoring and Modeling of Processes in the Soil-Plant-Atmosphere System |
会议日期 | JUN 19-21, 2013 |
会议地点 | Naples, ITALY |
英文摘要 | A shortage of rain and water resources exits in semi-arid and arid zones, necessitating the use of marginal water such as treated sewage water (TSW) for irrigation. These waters may contain substantial amounts of mixed-sodium-calcium salts, which, in turn, interact with the soil matrix. The soil solution-soil matrix (SS-SM) interactions, particularly in the presence of smectite minerals (e. g., montmorillonite), may change the soil pore-size distribution, and, consequently, could affect the soil hydraulic properties. Since the magnitude of the SS-SM interactions depends on time-dependent flow-controlled attributes, i.e., water content, pressure head, and solute concentrations, the resultant hydraulic properties are also time-dependent. Numerical simulations of flow and transport in a three-dimensional (3-D), spatially heterogeneous, variably saturated soil, for the case in which the flow is coupled to the transport through the dependence of the soil hydraulic properties on solute concentrations, were employed in order to analyze flow and transport in salt-affected soil. The case under consideration was a citrus orchard planted on a structured clay soil in a region characterized by a distinct rainy period during the winter and a relatively long dry season, requiring irrigations. Results of the analyses suggest that enhanced SS-SM interactions, induced by increasing soil exchangeable sodium during the irrigation season and dilution of the soil solution during the rain season, may considerably reduce soil hydraulic conductivity during the rain season, particularly, close to the soil surface. Consequently, enhanced SS-SM interactions, may slow down the solute movement, may substantially increase the tailing of the mean solute breakthrough at a given horizontal control plane (CP), and may lead to mean and standard deviation solute profiles which exhibit bimodal distributions, characterized by a substantial, secondary peaks close to the soil surface. Practical implications of this study regarding the long-term use of TSW for irrigation are briefly discussed. (C) 2013 The Authors. Published by Elsevier B.V. |
英文关键词 | unsaturated flow solute transport treated sewage water soil salinity |
来源出版物 | FOUR DECADES OF PROGRESS IN MONITORING AND MODELING OF PROCESSES IN THE SOIL-PLANT-ATMOSPHERE SYSTEM: APPLICATIONS AND CHALLENGES |
ISSN | 1878-0296 |
出版年 | 2013 |
卷号 | 19 |
页码 | 623-632 |
EISBN | ***************** |
出版者 | ELSEVIER SCIENCE BV |
类型 | Proceedings Paper |
语种 | 英语 |
国家 | Israel |
收录类别 | CPCI-S |
WOS记录号 | WOS:000326900300070 |
WOS关键词 | SATURATED HETEROGENEOUS SOIL ; FIELD-SCALE TRANSPORT ; INTERACTING SOLUTES ; NUMERICAL-ANALYSIS ; UNSATURATED SOILS ; SPATIAL VARIABILITY ; STOCHASTIC-ANALYSIS ; CONDUCTIVITY ; ZONE ; SYSTEM |
WOS类目 | Plant Sciences ; Environmental Sciences ; Soil Science |
WOS研究方向 | Plant Sciences ; Environmental Sciences & Ecology ; Agriculture |
资源类型 | 会议论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/302187 |
作者单位 | ARO, Inst Soils Water & Environm Sci, Bet Dagan, Israel |
推荐引用方式 GB/T 7714 | Russo, David. Consequences of salinity-induced-time-dependent soil hydraulic properties on flow and transport in salt-affected soils[C]:ELSEVIER SCIENCE BV,2013:623-632. |
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