摘要
针对河北平原季风气候和土壤冲积而成的多层次性构造特点,探讨了均质型和间层土壤水分分布和运行特征,在此基础上,提出不同土壤构造三种灌溉模式。(1)土壤质地中等或偏粘均质型常规灌溉模式;(2)土壤质地偏轻均质型少量多次灌水模式;(3)间层土壤少次常量灌溉模式。
Besed on the characteristics of monsoon climate and the behaviors of multiple soil layers formed by alltivitim in Hebei plain, this paper discusses water distri-bution and movement in homogeneous and heterogeneous soils,on the basis os whichthree kinds of irrigation modes for different soil formation are proposed:(1)conventional irrigation mode for soil texture with loamy and light clay;(2) irrigation mode withless water and more times for soil texture with light loamy homogeneous clay;and (3)irrigation mode with normal water and less time for heterogenous soil texture.
出处
《干旱地区农业研究》
CSCD
北大核心
1996年第1期3-9,共7页
Agricultural Research in the Arid Areas
基金
中国
加拿大合作研究"河北旱地农业"项目
关键词
土壤水分
土体构型
灌溉模式
河北平原
soil water distribution in farmland
operation law
different soil pro-files
irrigation mode
Hebei Plain