摘要
本文介绍利用中子仪测定水文地质参数包气带田间持水量和含水层变幅带给水度的原理与方法。用中子仪测定土壤水分含量和变化量,分析计算水文地质参数,所得结果与其它方法测定值相近,可以认为中子仪测定水文地质参数是一种新的手段和方法。
This article introduces a method for determining hydrogeological parameters such as the field capacity in zone of aeration and the specific yield in aquifer where water content is varied.To calculate the above parameters, water content in soil and its variety were measured by a neutron probe. This method is simple and the results are close to those obtained using other methods.
出处
《核技术》
CAS
CSCD
北大核心
1989年第4期233-236,共4页
Nuclear Techniques
