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民勤绿洲白刺灌丛沙堆不同演化阶段表面抗蚀性及其影响因素
引用本文:杜建会,严平,展秀丽,俄有浩.民勤绿洲白刺灌丛沙堆不同演化阶段表面抗蚀性及其影响因素[J].应用生态学报,2008,19(4):763-768.
作者姓名:杜建会  严平  展秀丽  俄有浩
作者单位:1. 北京师范大学资源学院防沙治沙教育部工程研究中心,北京,100875;北京师范大学中国沙漠研究中心,北京,100875
2. 甘肃省治沙研究所,甘肃武威,733000
基金项目:教育部跨世纪优秀人才培养计划 , 国家科技攻关项目 , 甘肃省荒漠化防治重点实验室开放基金
摘    要:通过测定甘肃民勤绿洲外围不同演化阶段灌丛沙堆表面抗剪强度,选取稳定阶段灌丛沙堆,定位观测结皮和植被去除前后灌丛沙堆表面侵蚀速率,研究了白刺灌丛沙堆表面抗蚀性及其影响因素,结果表明:稳定阶段灌丛沙堆土壤抗剪强度最大,在0.31~0.79 kg·cm-2,雏形阶段最小,在0.06~0.15 kg·cm-2,稳定阶段灌丛沙堆的土壤抗剪强度显著高于其它演化阶段(P<0.01);除退化阶段外,其它演化阶段不同坡位土壤抗剪强度差异均不显著(P>0.05).去除结皮和植被后,稳定阶段灌丛沙堆表面抗剪强度迅速下降,去除前后差异显著(P<0.01),去除后不同坡位差异不显著(P>0.05).保留结皮和植被,灌丛沙堆不同部位均出现堆积;去除结皮但保留植被,灌丛沙堆堆积量开始减小;去掉植被保留结皮,灌丛沙堆表面堆积量迅速减小;去除结皮和植被后,灌丛沙堆表面出现严重风蚀.

关 键 词:民勤  灌丛沙堆  结皮  土壤抗剪强度  民勤绿洲  白刺  灌丛沙堆  演化阶段  表面侵蚀速率  抗蚀性  影响因素  affecting  factors  related  Minqin  oasis  succession  different  风蚀  严重  积量  同部位  差异显著  强度差异  土壤抗剪强度  坡位
文章编号:1001-9332(2008)04-0763-06
收稿时间:2007-08-20
修稿时间:2007年8月20日

Surface erosion-resistance of Nitraria tangutorun nebkhas at different succession stages in Minqin oasis and related affecting factors
DU Jian-hui,YAN Ping,ZHAN Xiu-li,E You-hao.Surface erosion-resistance of Nitraria tangutorun nebkhas at different succession stages in Minqin oasis and related affecting factors[J].Chinese Journal of Applied Ecology,2008,19(4):763-768.
Authors:DU Jian-hui  YAN Ping  ZHAN Xiu-li  E You-hao
Institution:Engineering Center of Desertification and Blown-sand Control of Education Ministry, College of Resources Science and Technology, Beijing Normal University, Beijing 100875, China. dujh@ires.cn
Abstract:By measuring the surface shear strength of Nitraria tangutorun nebkhas at different succession stages in the fringe of Minqin oasis, and selecting several typical nebkhas at stabilizing stage to investigate its surface erosion rates before and after removing crust and vegetation, the surface erosion-resistance of N. tangutorun nebkhas and related affecting factors were studied. The results showed that the nebkhas had the highest surface shear strength (0.31-0.79 kg cm(-2)) at stabilizing stage, and the lowerest one (0.06-0.15 kg cm(-2)) at rudimental stage. The surface shear strength of nebkhas at stabilizing stage was significantly higher than that at other succession stages (P <0.01), and at the other succession stages except degradation stage, there was no significant difference in the surface shear strength in windward and leeward (P >0.05). After removing crust and vegetation, the surface shear strength of nebkhas at stabilizing stage was greatly reduced, with the difference before and after removing the crust and vegetation being significant (P <0.01). However, there was no obvious difference between different slope positions (P >0.05). Keeping both vegetation and crust, deposition occured on both slope positions of nebkhas; removing crust but keeping vegetation, the deposition reduced a little; removing vegetation but keeping crust, the deposition reduced greatly; while removing both vegetation and crust, nebkhas surface was severely eroded.
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