Arid
DOI10.1016/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
ISSN1878-0296
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/2XILL650/302421
作者单位ARO, Inst Soils Water & Environm Sci, Bet Dagan, Israel
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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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