ISWC OpenIR  > 水保所知识产出(1956---)
黄土丘陵区生物土壤结皮表面糙度特征及影响因素
王媛1,2; 赵允格2; 姚春竹1,2; 张培培2,3
2014
发表期刊应用生态学报
卷号25期号:3页码:647-656
摘要

地表糙度是影响地表径流和侵蚀过程的重要属性. 生物结皮在干旱半干旱区广泛分
布,是地表糙度的影响因子之一. 本文采用链条法测定了黄土丘陵区不同发育阶段生物结皮
表面糙度特征,分析了不同发育阶段生物结皮表面糙度对坡向、土壤含水量和冻融作用的响
应及其与各理化性质的相关性,初步探索了生物结皮对地表糙度的影响及其相关因素. 结果
表明: 生物结皮显著改变地表糙度,随着生物结皮从藻结皮向藓结皮演替,其糙度先降低后
增加,生物结皮发育形成10 年以后,其表面糙度基本趋于稳定; 研究区早期形成的藻结皮表
面糙度较裸土降低47. 0%,深色藻结皮( 藓类盖度< 20%) 较裸土降低20. 4%,混生结皮( 藓
类盖度为20% ~ 60%) 和苔藓结皮( 藓类盖度> 70%) 表面糙度与深色藻结皮基本一致; 坡向
对发育10 年以上的生物结皮表面糙度的影响不显著; 土壤含水量影响地表糙度特征. 研究区
浅色藻结皮表面糙度随水分变化较为剧烈; 随着生物结皮发育,深色藻结皮、混生结皮和苔藓
结皮表面糙度随水分的变化趋于平缓. 冻融增加了生物结皮表面糙度. 浅色藻结皮经两次冻
融后表面糙度增加29. 7%; 深色藻结皮、混生结皮和藓结皮表面糙度的影响需经过反复冻融
才有所体现. 生物结皮表面糙度与藓结皮盖度呈显著正相关( P < 0. 1) .

其他摘要

Soil surface roughness exerts profound influence on runoff and sediments yield from
slopes. Biological soil crusts ( BSCs) are ubiquitous living cover in the open spaces between plants
in arid and semiarid ecosystems,which considerably impact the surface roughness. Aimed to determine
the effect of biological crusts on the surface roughness and its influence factors,this study investigated
the surface roughness of soil with BSCs at their different successional stages by using the
chain method. Besides,the impacts of slope aspects,soil water content and freezing and thawing on
surface roughness were also investigated. Then,the correlations between roughness and soil chemical
and physical properties were evaluated. The results showed that soil surface roughness decreased
at the initial successional stage of BSCs but increased along with BSCs’development in the region.
Soil roughness tended to be stabile since BSCs developed ten years later. The roughness was reduced
by 47. 0% by the light cyanobacteria-dominated crust and 20. 4% by the dark cyanobacteriadominated
crust ( moss coverage < 20%) ,compared with the bare soil. Soil moisture significantly
impacted surface roughness. The surface roughness of BSCs changed obviously with soil moisture in
the early development,but only slightly in their later succession. Freezing-thawing also affected
surface roughness with BSCs. Roughness was more susceptible to freezing-thawing in the early de-velopment of BSCs,with an increase of 29. 7% compared with the bare soil. The surface roughness
of late successional BSCs exhibited a slight change only after repeated freezing-thawing. The surface
roughness of BSCs showed a statistically significant relationship with the coverage of moss ( P <
0. 1) .

关键词生物土壤结皮 发育阶段 生物结皮表面糙度 影响因子 黄土丘陵区
收录类别中文核心期刊要目总览
语种中文
文献类型期刊论文
条目标识符sbir.nwafu.edu.cn/handle/361005/9659
专题水保所知识产出(1956---)
作者单位1.西北农林科技大学资源环境学院
2.中国科学院大学
3.西北农林科技大学水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室
推荐引用方式
GB/T 7714
王媛,赵允格,姚春竹,等. 黄土丘陵区生物土壤结皮表面糙度特征及影响因素[J]. 应用生态学报,2014,25(3):647-656.
APA 王媛,赵允格,姚春竹,&张培培.(2014).黄土丘陵区生物土壤结皮表面糙度特征及影响因素.应用生态学报,25(3),647-656.
MLA 王媛,et al."黄土丘陵区生物土壤结皮表面糙度特征及影响因素".应用生态学报 25.3(2014):647-656.
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