首页 | 本学科首页   官方微博 | 高级检索  
     检索      

黄土高原土壤干层减缓方法初探
引用本文:杨建军,李会科,张广军,吕光辉,师庆东,塔西甫拉提·特依拜,YANG Jian-jun,LI Hui-ke,ZHENG Guang-jun,Lü Guang-hui,SHI Qing-dong,Taxifulati.Teyibai.黄土高原土壤干层减缓方法初探[J].水土保持学报,2006,20(4):186-190.
作者姓名:杨建军  李会科  张广军  吕光辉  师庆东  塔西甫拉提·特依拜  YANG Jian-jun  LI Hui-ke  ZHENG Guang-jun  Lü Guang-hui  SHI Qing-dong  Taxifulati.Teyibai
作者单位:1. 新疆大学,资源与环境科学学院,新疆,乌鲁木齐市,830046;新疆大学,绿洲生态重点实验室,新疆,乌鲁木齐市,830046
2. 西北农林科技大学,资源与环境学院,陕西,杨陵,712100
3. 新疆大学,资源与环境科学学院,新疆,乌鲁木齐市,830046
基金项目:中国科学院知识创新工程项目;新疆大学校科研和教改项目
摘    要:针对黄土高原长期种植苜蓿会导致深层土壤的干层化现象,在陕北黄土丘陵沟壑区的苜蓿种植区采用侧膜种植、播量减半种植、间作种植、常规种植4种种植模式来分析土壤水分环境。研究表明:侧膜种植年内贮水量在各个时期较其它3种模式高,各种植模式有效降雨量与土壤水分补给量之间关系呈线性相关,侧膜种植提高0~180cm土层土壤水分补给量更为突出。有效降雨对4种种植模式活跃层的贮水补偿作用极显著。春夏失墒期各种模式土壤相对稳定层对活跃层的补偿作用显著,各处理的相对稳定对活跃层补给量之间呈直线正相关,但补给量存在一定差异。

关 键 词:黄土高原  土壤干层  苜蓿  土壤水分
文章编号:1009-2242(2006)04-0186-05
收稿时间:2006-04-26
修稿时间:2006-04-26

Preliminary Research on Countermeasures of Desiccation of Deep Soil Layer in Loess Plateau
YANG Jian-jun,LI Hui-ke,ZHENG Guang-jun,SHI Qing-dong,Taxifulati.Teyibai.Preliminary Research on Countermeasures of Desiccation of Deep Soil Layer in Loess Plateau[J].Journal of Soil and Water Conservation,2006,20(4):186-190.
Authors:YANG Jian-jun  LI Hui-ke  ZHENG Guang-jun  SHI Qing-dong  TaxifulatiTeyibai
Abstract:Alfalfa is often planted perennially in the Loess Plateau,which leads to the desiccation of deep soil layer.So,alfalfa is planted with four different patterns to lessen the formation of dried soil layer,which includes the halve sowing establishment,the intercrop establishment,the plastic film mulching establishment and the check establishment.The main results showed: the water storage of the plastic film mulching establishment was higher than the other three establishments in any time of the year.There is a very significant linear dependence between the available rainfall and replenishment of the soil water.The replenishment of plastic film mulching establishment is more obviously than the othr three establishments.The available rainfall replenish the active layer significantly.During the transition from spring to summer,the stable layer replenish the active layer significantly.There is a very significant linear dependence between the replenishment of stable layer and active layer of four establishments,but replenishments are different.
Keywords:the Loess Plateau  dried soil layers alfalfa  soil water
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《水土保持学报》浏览原始摘要信息
点击此处可从《水土保持学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号