潮间带土壤盐度与电导率的关系  

Relation between soil salinity in intertidal zone and electric conductivity

作　　者：张瑜斌[1] 邓爱英[1] 庄铁诚[1] 林鹏[1] 

机构地区：[1]厦门大学生命科学学院

出　　处：《生态环境》2003年第2期164-165,共2页Ecology and Environmnet

基　　金：国家自然科学基金项目(30270272)

摘　　要：以5∶1的水土质量比浸提潮间带土壤,质量法测定的土壤盐度(质量分数),与电导法测定的稀释了5倍的土壤浸提液(5∶1水土质量比)的电导率值之间有极显著的相关性。质量法实测的土壤盐度与电导率计算的土壤盐度之间的相对误差多在5%以下。因此,用电导法测定潮间带土壤盐度不失为一种简便、快速的方法,尤其是样品数较多时更可节约时间。There was significantly correlation between soil salinity in intertidal zone obtained by mass method (the ratio of mass of water to soil is 5∶1) and electric conductivity of extracting solution diluted five times by electric conductivity method The relative errors were almost below 5% between soil salinity measured by the mass method and the ones calculated by electric conductivity. So, electric conductivity method is a simple and rapid method for measurement of soil salinity in intertidal zone after defining the regression equation between soil salinity and electric conductivity. Plenty of time can be saved by electric conductivity method when soil samples are excessive.

关 键 词：潮间带 土壤 盐度 电导率 电导法 

分 类 号：S151.9[农业科学—土壤学]