自然科学版
陕西师范大学学报(自然科学版)
资源与环境科学
前期旱情等级对红壤坡面土壤裂缝及产流产沙特征的影响
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陈晓安
(江西省水土保持科学研究院, 江西省土壤侵蚀与防治重点实验室, 江西 南昌 330029)
陈晓安,男,工程师,主要研究方向为土壤侵蚀机理。E-mail:onlycxa@163.com
摘要:
在人工模拟试验的基础上,采用图片处理技术和统计分析方法,分析无旱、轻旱、中旱、重旱4种旱情级别下的坡面土壤裂缝特征以及前期干旱影响下的坡面产流产沙特征。结果表明:土壤裂缝长度密度、面积密度、宽度、裂缝交点数、土壤裂缝弯曲度从小到大依次为轻旱、中旱、重旱;土壤裂缝条数从轻旱到中旱略有下降,到重旱后土壤裂缝数量激增,土壤裂缝网络的连通性从轻旱到中旱急剧增大,中旱到重旱基本一致。轻旱、中旱、重旱下土壤产流开始时间比无旱土壤分别增加1.83、2.43、3.87 min,产流截止时间比无旱土壤分别减少0.97、1.23、1.40 min;无旱、轻旱、中旱、重旱土壤产流稳定前各时段产流量依次减小,稳定后无明显差异,总产流量随旱情等级加大而减小。土壤平均产沙浓度从无旱、轻旱、中旱依次增加,中旱到重旱有所减小,稳定前土壤产沙速率从轻旱到重旱依次减小,无旱土壤最小,从无旱到重旱总侵蚀产沙先增大后减小,轻旱、中旱、重旱土壤侵蚀量分别是无旱的3.92、3.85、2.50倍。
关键词:
干旱等级; 红壤; 土壤裂缝; 水土流失
收稿日期:
2015-07-06
中图分类号:
F294.3
文献标识码:
A
文章编号:
1672-4291(2015)06-0089-05doi:10.15983/j.cnki.jsnu.2015.06.464
基金项目:
江西省水利科技重大项目(KT201109);江西省水利科技项目(KT201419); 江西省优势科技创新团队(20152BCB24011)
Doi:
Effects of pre-dry grade on soil cracks and characteristics of runoff and sediment in red soil slopes
CHEN Xiaoan
(Jiangxi Institute of Soil and Water Conservation, Key Laboratory of Soil Erosion and Prevention, Nanchang 330029, Jiangxi, China)
Abstract:
Based on artificial stimulation experiment, soil crack characteristics and runoff and sediment yields under different drought grades such as no drought, slight drought, medium drought and severe drought have been investigated with the help of photograph processing and statistical methods.The results suggested that soil crack length density, area density, width, intersection and curvature increased with the increasing of drought grade. In addition, the number of soil crack under slight drought was slightly less than medium drought, but much less than severe drought. Soil crack connectivity sharply increased from slight drought to medium slight with no differences between medium slight and severe drought. The starting time of runoff yield under slight drought, medium drought and severe drought increased by 1.83, 2.43 and 3.87 min than no drought, respectively, but the ending time decreased by 0.97, 1.23 and 1.40 min, respectively. Before stabilization of runoff producing, the runoff yields increased with increasing of drought grades, but there were no differences after stabilization of runoff. Total runoff yields decreased as the increase of drought grades. Average soil runoff yields increased from no drought to medium drought, but slightly decreased from medium drought to severe drought. Before stabilization of runoff producing, sediment yields decreased from slight drought to severe drought, with lowest sediment yields under no drought. Total sediment yields firstly increased and then decreased with the increase of drought grades. Total sediment yield under slight drought, medium drought and severe drought were 3.92, 3.85 and 2.50 times of that under no drought respectively.
KeyWords:
drought grade; red soil; soil crack; soil and water losses