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作 者:张鹏辉[1] 王健[1] 马璠[2] 刘振[1] 李鹤[1] 李鹏飞[1]
机构地区:[1]西北农林科技大学资源环境学院,陕西杨凌712100 [2]宁夏农林科学院荒漠化治理研究所,银川750002
出 处:《中国农村水利水电》2014年第7期7-9,共3页China Rural Water and Hydropower
基 金:国家自然科学基金(41101268);西北农林科技大学青年专项基金(QN2011152)
摘 要:土壤的抗侵蚀能力包括土壤的抗冲性和抗蚀性。根系的固结缠绕对土壤的抗侵蚀能力具有显著的影响。以不同含量的冬小麦根系的土样为研究对象,采用静水崩解法和抗冲槽法测定其抗冲性和抗蚀性。结果表明:根系能够降低土壤的崩解速率,即随着根系含量的增加,土壤崩解率缓慢降低。研究结果显示:土壤崩解过程可以分为吸水崩解阶段、快速崩解阶段、稳定崩解阶段3个阶段,随根密度增加,根系作用延长了土壤吸水崩解和快速崩解阶段,降低了土壤崩解速度。土壤抗冲刷系数随着根重密度的增加呈递增的二次函数关系。The soil erosion resistance includes soil antl-scourablllty and antl-erocllDlllty. The consolidation and winding of roots have asignificant impact on soil erosion resistance. In this paper, we study the anti-scourability and anti-erodibility of soil samples of winter wheat roots at different levels by using the hydrostatic disintegration method and the soil bins method. The results show that: the roots can decrease the soil disintegration rate and that it is slowly decreasing with the increase in the roots. The process of disintegra- tion can be divided into absorbent disintegration stage, rapid disintegration and steady disintegration stage. The absorbent disintegra- tion and rapid disintegration have become long with the increase in roots density. It shows an increments quadratic function relation- ship between the soil anti-scourability coefficient and root weight density.
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