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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:土壤盐分模拟是有效控制盐碱化和区域盐碱化土地利用的基础。本文以黄河三角洲地区的脆弱变量为基础,利用脚踏传递函数(PTF)和地理信息系统(GIS)技术模拟了土壤盐分的动态变化。通过对5月至10月植物生长期间黄河三角洲三种土壤类型的土壤盐分,EC和地下水水位的现场观测数据以及地下水的实时降水和蒸发量进行多元线性回归分析,得出了模拟模型。利用GIS根据回归模型模拟了土壤盐分的时空变化。结果表明,尽管理论上不能完全解释线性回归模型,但它们是可行的。土壤盐分的动态变化基于前期的变化,前期的土壤盐分在下一阶段的变化中起着最大的作用。滩区受潮汐和海水浸泡的土壤盐分较高而相对稳定,内陆地区的盐分在季节降雨,蒸发和地下水方面已发生变化。

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