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作 者:钟兆站[1] 赵聚宝[1] 薛军红[1] 梅旭荣[1]
机构地区:[1]中国农业科学院农业气象研究所
出 处:《中国农业气象》1996年第3期1-6,共6页Chinese Journal of Agrometeorology
摘 要:利用压力膜方法测定晋中东山地区褐土的土壤水分,并分析了土壤水分及其能态特征。结果表明:本区土壤水吸力与土壤含水量之间呈明显的幂函数关系,可以用幂函数方程模拟;土壤的当量孔径分布大致随土壤水吸力的增加而减小;土壤的结构性能良好,通气孔隙、毛管孔隙、无效孔隙的当量孔径分布分别占土壤总孔隙度的18.3%、51.2%和30.5%,尤其是毛管孔隙的分布占土壤总孔隙度的一半以上;土壤的比水容量随吸力的增大而迅速减小.当吸力为0.1×10 ̄5~0.3×10 ̄5pa时,其比水容量的量级为10 ̄(-1)[m1/(10 ̄5pa·g)],而当吸力达3×10 ̄5~15×10 ̄5pa时,其比水容量的量级下降了100倍,为10 ̄(-3)[ml/(10 ̄5Pa·g)]。表层土壤水分对于作物吸收利用比心土层和底土层更为有效,但深层土壤的持水性能比表层士壤要好。为此,必须提高作物对土壤深层储水的利用。Uscd by the pressure membrane method,determined the soil water characteristic curve of cinna-mon soil in the east mountainous areas of middle Shanxi province,and analyzed the dynamic charac-teristic of soil water energy,The results show that in these areas.the relationship between the soil suc-tion and the soil water content could be simulated with the power function;the distribution of soil e-qu ivalent pore diameter decreases as the soil suction increases,the porcentage of soil equivalent porediameter of aeration porcoity, capillary porcoity and inactive porcaity to total soil porosity is 18.3%,51.2%and 30.5%respectively,which that means the soil in these areas has a good structure andfunction,especially the soil capillary porosity takes up over half of the total soil porosity,which pro-vides the soil with a favorable condition for the soil water storage,soil moisture maintenance and ef-fective crop utilization to soil water; specific soil water capacity decreases rapidly as the soil suction in-creases , the dimension degree of specific soil water capacity is 10-1(ml/105pa·g)when the soil suc-tion is 0.1×105~0. 3× 105pa, and 10-3(ml/105pa·g)when soil suction is 3× 105~15× 105pa. Thewater in topsoil is more effective than that in subsoil and undersoil, whereas the water retention a-bility of undersoil is greater than that of topsoil,which indicates that the water held in undersoil mustbe utilized futther,in order to ensure agriculture in these dry farming areas develop in a sustainable,steady way.
分 类 号:S155.25[农业科学—土壤学] S152.7[农业科学—农业基础科学]
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