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Simulating Temporal and Spatial Changes of Soil Salinity in Yellow River Delta, China Using GIS

机译:基于GIS的黄河三角洲土壤盐分时空变化模拟。

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Simulation of soil salinity is the basis for effective control of salinization and utilization of regional salinization lands. This paper was to simulate dynamic of soil salinity with pedo-transfer functions (PTFs) and geographic information system (GIS) technology based on facile variables in Yellow River Delta. Simulating models were derived from field observation data of soil salinity, EC and water table of groundwater, and real time rainfall and evaporation through multiple linear regression analysis for three soil types in Yellow River Delta during time from May to October when plants grows. The temporal and spatial changes of soil salinity were simulated according to regression models using GIS. The results presented that linear regression models were practicable though they can not be completely explained in theory. The dynamic changes of soil salinity were based on that of prophase and the soil salinity of prophase had played uppermost role in that of next phase. The soil salinity, affected by tides and soaked by seawater, in beach zone is high and steady relatively and that of inland had been changed in terms of regional rainfall, evaporation and groundwater in seasons.
机译:土壤盐度模拟是有效控制盐渍化土地盐渍化和利用的基础。本文是根据黄河三角洲的宽松变量模拟土壤盐度的动态和地理信息系统(GIS)技术。仿真模型源自地下水土壤盐度,EC和水表的现场观测数据,以及通过多种线性回归分析,从5月到10月在植物生长时从五月到十月的三种土壤类型的多元线性回归分析蒸发。根据使用GIS的回归模型模拟土壤盐度的时间和空间变化。结果呈现了线性回归模型,尽管它们无法完全解释理论上。土壤盐度的动态变化是基于预先存在的,并且预先存在的土壤盐度在下一阶段发挥了最高作用。海滩区受到潮汐影响的土壤盐度,海滩区的潮湿,相对稳定,在区域降雨,蒸发和地下水中,内陆的变化。

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