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

黄河三角洲滩地不同植被类型的土壤贮水功能
引用本文:夏江宝,陆兆华,高鹏,许景伟,李传荣.黄河三角洲滩地不同植被类型的土壤贮水功能[J].水土保持学报,2009,23(5).
作者姓名:夏江宝  陆兆华  高鹏  许景伟  李传荣
作者单位:1. 山东省黄河三角洲生态环境重点实验室,滨州学院,山东,滨州,256603
2. 山东省黄河三角洲生态环境重点实验室,滨州学院,山东,滨州,256603;山东农业大学林学院,山东,泰安,271018
3. 山东省林业科学研究院,山东,济南,250014
4. 山东农业大学林学院,山东,泰安,271018
基金项目:国家科技支撑计划,山东省黄河三角洲生态环境重点实验室开放基金,山东省自然科学基金,滨州学院重大课题
摘    要:以滩涂裸地为对照,对黄河三角洲滩地乔木林、灌木林、草地及农田等4种植被类型改良土壤的盐碱程度、容重和孔隙度状况、土壤入渗性能及蓄水能力进行对比研究.结果表明:不同植被类型均具有一定的压碱抑盐效应.且表土层盐碱含量多低于20-40 cm土层;同时降低土壤容重,增加土壤孔隙度的效应显著,并且对土壤表层的改良效果好于20-40 cm土层.不同植被类型均能改善土壤入渗性能.渗透性能由强到弱表现为乔木林>灌木林>农田>草地,其平均渗透速率分别是滩涂裸地的4.9,3.7,2.9,1.9倍.不同植被类型的土壤饱和蓄水量、毛管蓄水量、非毛管蓄水量均表现为乔木林>灌木林>草地>农田,其饱和蓄水量分别比滩涂裸地高18.3%,11.8%,3.7%和3.5%;土壤涵蓄降水量和有效涵蓄量大小均表现为乔木林>草地>灌木林>农田,且0-20 cm土层的贮水性能均好于20-40 cm.

关 键 词:黄河三角洲  植被类型  土壤蓄水能力  土壤入渗

Soil Water Storage Ability of Different Vegetation Types in Lowlands of the Yellow River Delta
XIA Jiang-bao,LU Zhao-hua,GAO Peng,XU Jing-wei,LI Chuan-rong.Soil Water Storage Ability of Different Vegetation Types in Lowlands of the Yellow River Delta[J].Journal of Soil and Water Conservation,2009,23(5).
Authors:XIA Jiang-bao  LU Zhao-hua  GAO Peng  XU Jing-wei  LI Chuan-rong
Abstract:Compared with beaches bare land, characteristics of soil pH value, soil salt content, soil density and porosity, soil infiltration and water-holding of four kinds of, trees, shrubs, grassland and farmland vegetation are researched in lowlands of the Yellow River delta. Results indicate that; different vegetation types has obvious function of controlling soil salinity and alkaline content, and these indexes of 0-20 cm are less than that of 20-40 cm. The soil density decreased, and soil total porosity increased with different vegetation types, and these indexes of 0-20 cm are better than that of 20-40 cm. Soil infiltration capacity in different vegetation types are better than that in bare land, and the average penetration rate of trees , shrubs, grassland and farmland is 4. 9, 3. 7,2. 9,1. 9 times respectively, larger than that of bare land(0. 48 mm/min). Characteristics of soil saturated water content, soil capillary, non-capillary porosity water-holding capacity show this order: trees>shrubs>grassland>farmland, and compared with bare land, soil saturated water content enlargement is 18. 3%, 11. 8%, 3. 7%, 3. 5%. Soil total absorption precipitation and effective precipitation show this order; trees>grassland>shrubs >farmland>bare land, and soil water-holding capacity in 0-20 cm is better than that of 20-40 cm.
Keywords:Yellow River Delta  vegetation types  soil water-holding capacity  soil infiltration
本文献已被 万方数据 等数据库收录!
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