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Analysis of soil resistivity characteristics under meteorological conditions in Haikou City

机译:海口市气象条件下土壤电阻率特征分析

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Analysis of soil resistivity in Haikou City for nearly one year, the soil moisture data, and the meteorological data information provided by automatic meteorological station, the results show that soil resistivity of Haikou shows the distribution features of the east side lower than the west; soil resistivity of volcanic ash soil changes in inverse u-shaped curve with the seasons, while the red soil and sand soil resistivity changes with the seasons in u-shaped curve, and soil resistivity of the volcanic ash is not reduced due to the rainy season, instead it increases; soil resistivity of volcanic ash rises with the increase of soil humidity, while the soil resistivity of red soil and sand soil decreases with the increase of soil humidity. The soil resistivity of volcanic ash and red soil decreases with the increase of soil temperature, while the soil resistivity of sand soil rises with the increase of soil temperature. The soil resistivity of volcanic ash and red soil rises with precipitation, while soil resistivity of sand and red soil rises with precipitation. The decline of red soil was most pronounced.
机译:通过对海口市近一年的土壤电阻率进行分析,土壤湿度数据以及自动气象站提供的气象数据信息,结果表明,海口市土壤电阻率呈现出东侧比西侧低的分布特征。火山灰的土壤电阻率随季节呈反U型曲线变化,红壤和沙土的土壤电阻率随U型曲线呈季节变化,且雨季不会降低火山灰的土壤电阻率。 ,而是增加;火山灰的土壤电阻率随土壤湿度的增加而升高,而红壤和沙土的土壤电阻率随土壤湿度的增加而降低。火山灰和红壤的土壤电阻率随土壤温度的升高而降低,而沙土的土壤电阻率随土壤温度的升高而升高。火山灰和红壤的土壤电阻率随降水量增加,而沙和红壤的土壤电阻率随降水量增加。红土的减少最为明显。

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