摘要
对比分析了旱作免耕农田、传统翻耕农田、冬小麦地、退耕草地(苜蓿地)和柠条林地地表粗糙度、风蚀量及其与地表附着物相关性等土壤可蚀性差异。结果表明:旱作传统翻耕农田就地起沙量最大,土壤可蚀性最小,是当地沙尘的主要来源之一;免耕、退耕草地和柠条林地都能有效减少地表风蚀,土壤可蚀性明显较强;传统翻耕农田、冬小麦地风蚀颗粒主要集中在近地表,为就地起沙;提高"杂草频度"即植被覆盖率,对有效防治就地起沙、提高土壤可蚀性效果明显。
We studies and comparative analysis of different field use types about soil erodibility and its surface roughness(Z0),wind erosion quantity and its correlation with surface fixtures in no-tillage field,the traditional tillage field,winter wheat field,the returning farmland to grassland(alfalfa) and shrub(Caragana Fabr.) field. Observation we can see the traditional tillage field wind erosion is the most seriously,also soil erodibility is the least,is a major source of local dust storm.No-tillage,the returning farmland to grassland field,shrub field can be effective in reduces wind erosion,soil erodibility capacity also increases significantly.The mainly erosion field of conventional tillage fields,winter wheat are concentrate in the near-surface,it is belongs near-surface sand erosion.Improvement"weeds-frequency degree"that is,vegetation coverage can increases soil erodibility and prevents soil erosion obviously in arid area.
出处
《中国农学通报》
CSCD
北大核心
2010年第3期196-201,共6页
Chinese Agricultural Science Bulletin
基金
国家林业科技支撑"宁夏河东沙地退化草地植被恢复与利用技术研究与试验示范(盐池)"项目(2006BAD26B0702)
宁夏回族自治区科技厅"5183"治沙专项
关键词
宁夏中部干旱带
土壤可蚀性
集沙量
Ningxia middle arid area
soil erodibility
sand quantity