[1]FENG Wei,YE Jing.Effects of Biological Soil Crusts on Infiltration and Soil and Water Conservation Under Trample Disturbance[J].Research of Soil and Water Conservation,2016,23(01):34-37,43.
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Effects of Biological Soil Crusts on Infiltration and Soil and Water Conservation Under Trample Disturbance

References:
[1] 李金峰,孟杰,叶菁,等.陕北水蚀风蚀交错区生物结皮的形成过程与发育特征[J].自然资源学报,2014,29(1):67-79.
[2] 李聪会,朱首军,陈云明,等.黄土丘陵区生物结皮对土壤抗蚀性的影响[J].水土保持研究,2013,20(3):6-10.
[3] Bowker M A, Miller M E, Belnap J, et al. Prioritizing conservation effort through the use of biological soil crusts as ecosystem function indicators in an arid region[J]. Conservation Biology, 2008,22(6):1533-1543.
[4] 孟杰,卜崇峰,赵玉娇,等.陕北水蚀风蚀交错区生物结皮对土壤酶活性及养分含量的影响[J].自然资源学报,2010,25(11):1864-1874.
[5] 肖波,赵允格,许明祥,等.陕北黄土区生物结皮条件下土壤养分的积累及流失风险[J].应用生态学报,2008,19(5):1019-1026.
[6] 赵建成,张丙昌,张元明.新疆古尔班通古特沙漠生物结皮绿藻研究[J].干旱区研究,2006,23(2):189-194.
[7] 高丽倩,赵允格,秦宁强,等.黄土丘陵区生物结皮对土壤可蚀性的影响[J].应用生态学报,2013,24(1):105-112.
[8] 唐克丽.黄土高原水蚀风蚀交错区治理的重要性与紧迫性[J].中国水土保持,2000,224(11):11-12.
[9] 李莉,孟杰,杨建振,等.不同植被下生物结皮的水分入渗与水土保持效应[J].水土保持学报,2010,24(5):105-109.
[10] 张侃侃,卜崇峰,高国雄.黄土高原生物结皮对土壤水分入渗的影响[J].干旱区研究,2011,28(5):808-812.
[11] 孟杰.黄土高原水蚀交错区生物结皮的时空发育特征研究[D].陕西杨凌:西北农林科技大学,2011.
[12] 肖波,赵允格,邵明安.黄土高原侵蚀区生物结皮的人工培育及其水土保持效应[J].草地学报,2008,16(1):28-33.
[13] 成向荣,黄明斌,邵明安.神木水蚀风蚀交错带主要人工植物细根垂直分布研究[J].西北植物学报,2007,27(2):321-327.
[14] 路炳军,袁爱萍,章文波.径流小区集流桶(池)泥沙含量快速测定方法探讨[J].水土保持通报,2009,29(2):15-17.
[15] 熊好琴,段金跃,王妍,等.毛乌素沙地生物结皮对水分入渗和再分配的影响[J].水土保持研究,2011,18(4):82-87.
[16] 张玉斌,郑粉莉.近地表土壤水分条件对坡面土壤侵蚀过程的影响[J].中国水土保持科学,2007,5(2):5-10.
[17] 秦宁强.黄土丘陵区生物土壤结皮对降雨侵蚀力的响应及影响[D].陕西杨凌:西北农林科技大学,2012.
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