检索规则说明:AND代表“并且”;OR代表“或者”;NOT代表“不包含”;(注意必须大写,运算符两边需空一格)
检 索 范 例 :范例一: (K=图书馆学 OR K=情报学) AND A=范并思 范例二:J=计算机应用与软件 AND (U=C++ OR U=Basic) NOT M=Visual
作 者:胡江波[1] 杨改河[1] 贺桂芹[2] 张笑培[2] 刘志超[1] 淮宗安 李会萍
机构地区:[1]西北农林科技大学农学院 [2]西北农林科技大学资源环境学院 [3]千阳县林业工作站,陕西千阳721500
出 处:《中国水土保持》2007年第10期29-31,共3页Soil and Water Conservation in China
基 金:国家重大基础预研项目(2005CCA05300)
摘 要:采用野外调查、定点观测与室内分析相结合的方法,对渭北旱塬丘陵沟壑区不同植被恢复模式(A组为刺槐林1和荒坡,B组为封育和未封育,C组为刺槐林2和农田)土壤水分的变化规律进行了研究。结果表明,不同植被恢复模式土壤水分的季节动态变化趋势基本一致,近似于抛物线形,但也存在一定的差异。10月份以前,A、B两组植被恢复模式的土壤含水量均小于对照,此后较对照明显提高,说明在降水较少的月份,尤其是旱季,保水效果好;C组中,刺槐林2土壤含水量表现出和农田基本相似的变化趋势,且土壤含水量始终较农田高。3组不同植被恢复模式土壤水分平均值总体上随土层深度的增加而逐渐增加,当年降水对土壤水分的补偿作用均较好;其变异系数总体上随着土层的增加而逐渐减小;3组不同植被恢复模式不同层次土壤水分的变化幅度差异较大,随着土层深度的加大,土壤水分含量随时间的变化幅度呈减少趋势。The paper studies the variation law of soil moisture of different vegetation rehabilitation modes(Group A:locust trees1 + waste slopes,Group B:closing hillsides to facilitate afforestation + non-closing hillsides to facilitate afforestation,Group C:locust trees2 + farmland)of gullied rolling loess area in the north of arid table land of the Weihe River by using the combined method of field survey,fixed point observation and indoor analysis.The outcomes show that the seasonal dynamic variation trend of soil moisture in different vegetation rehabilitation modes is basically the same and approximates a parabolic shape,but it still exists a certain difference.Before October,the soil moisture of vegetation rehabilitation mode of Groups A and B is all smaller than that of the check and obviously increased thereafter,showing that is in the dry months,especially during the dry season,the effect of water conservation is good.In Group C,the variation trend of soil moisture of locust trees2 is similar with that of the farmland and the soil moisture is always higher than that of the farmland.The mean value of soil moisture of different vegetation rehabilitation modes of three groups is gradually increased along with the increase of soil depth and the same year precipitation has better function of soil moisture compensation;the coefficient of variation is gradually reduced along with the increase of soil layer and;the variation range of soil moisture in different layers of different vegetation rehabilitation modes of the three groups is great and is in the trend of reduction along with the time and the increase of soil depth.
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在链接到云南高校图书馆文献保障联盟下载...
云南高校图书馆联盟文献共享服务平台 版权所有©
您的IP:216.73.216.26