首页> 外文会议>Groundwater-Present Status and Future Task >THE DYNAMIC CHANGE OF SOIL WATER AND ITS FACTORANALYSIS IN THE LOW PLAIN OFWESTERN JILIN PROVINCE
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THE DYNAMIC CHANGE OF SOIL WATER AND ITS FACTORANALYSIS IN THE LOW PLAIN OFWESTERN JILIN PROVINCE

机译:吉林省西部低平原区土壤水的动态变化及其因子分析。

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摘要

According to a lot of dynamic monitoring data of precipitation, soil water, groundwater and surface water, the temporalrnand spatial variation law of soil water (or soil moisture) content and its influencing factors in the western plain area of Jilin Provincernare analyzed. It is thought that relationships existed in the spatial distribution of soil water content with formation's character;rndifferent target year and different months, the soil water content is different; generally, surface soil water content increases graduallyrnfrom June to July, soil water moves downward, and it decreases in August to September. Influencing factors of soil water contents arernthe climate, geological conditions, irrigation, groundwater level and geographic environment. Among these, precipitation is the masterrnelement, geological conditions are the factors controlled by the space, and irrigation, groundwater level and geographic environmentrnare influencing factors.
机译:根据大量降水,土壤水,地下水和地表水的动态监测数据,分析了吉林省西部平原地区土壤水(或土壤水分)含量的时空变化规律及其影响因素。认为土壤含水量的空间分布与地层性状之间存在着联系;不同的目标年份和不同的月份,土壤含水量是不同的。一般而言,6月至7月,地表土壤含水量逐渐增加,土壤水分向下移动,8月至9月减少。土壤含水量的影响因素是气候,地质条件,灌溉,地下水位和地理环境。其中,降水是主要控制因素,地质条件是受空间控制的因素,灌溉,地下水位和地理环境是影响因素。

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