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苔藓为主的生物结皮与植被对侵蚀及土壤水分的综合影响及其对中国黄土高原干扰的启示

The combined effects of moss-dominated biocrusts and vegetation on erosion and soil moisture and implications for disturbance on the Loess Plateau, China.

作者信息

Bu Chongfeng, Wu Shufang, Han Fengpeng, Yang Yongsheng, Meng Jie

机构信息

Northwest A & F University, State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Yangling, Shaanxi, China; Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi, China.

College of Water Resources and Architectural Engineering, Northwest A & F University, Yangling, Shaanxi, China.

出版信息

PLoS One. 2015 May 20;10(5):e0127394. doi: 10.1371/journal.pone.0127394. eCollection 2015.

Abstract

Biological soil crusts (BSCs, or biocrusts) have important positive ecological functions such as erosion control and soil fertility improvement, and they may also have negative effects on soil moisture in some cases. Simultaneous discussions of the two-sided impacts of BSCs are key to the rational use of this resource. This study focused on the contribution of BSCs while combining with specific types of vegetation to erosion reduction and their effects on soil moisture, and it addressed the feasibility of removal or raking disturbance. Twelve plots measuring 4 m × 2 m and six treatments (two plots for each) were established on a 15° slope in a small watershed in the Loess Plateau using BSCs, bare land (as a control, BL), Stipa bungeana Trin. (STBU), Caragana korshinskii Kom. (CAKO), STBU planted with BSCs (STBU+BSCs) and CAKO planted with BSCs (CAKO+BSCs). The runoff, soil loss and soil moisture to a depth of 3 m were measured throughout the rainy season (from June to September) of 2010. The results showed that BSCs significantly reduced runoff by 37.3% and soil loss by 81.0% and increased infiltration by 12.4% in comparison with BL. However, when combined with STBU or CAKO, BSCs only made negligible contributions to erosion control (a runoff reduction of 7.4% and 5.7% and a soil loss reduction of 0.7% and 0.3%). Generally, the soil moisture of the vegetation plots was lower in the upper layer than that of the BL plots, although when accompanied with a higher amount of infiltration, this soil moisture consumption phenomenon was much clearer when combining vegetation with BSCs. Because of the trivial contributions from BSCs to erosion control and the remaining exacerbated consumption of soil water, moderate disturbance by BSCs should be considered in plots with adequate vegetation cover to improve soil moisture levels without a significant erosion increase, which was implied to be necessary and feasible.

摘要

生物土壤结皮(BSCs,或称为生物结皮)具有重要的积极生态功能,如控制侵蚀和提高土壤肥力,不过在某些情况下它们也可能对土壤湿度产生负面影响。同时探讨生物土壤结皮的双面影响是合理利用这一资源的关键。本研究聚焦于生物土壤结皮与特定植被类型相结合时对减少侵蚀的贡献及其对土壤湿度的影响,并探讨了去除或耙动干扰的可行性。在黄土高原一个小流域的15°斜坡上,利用生物土壤结皮、裸地(作为对照,BL)、本氏针茅(STBU)、柠条锦鸡儿(CAKO)、种植了生物土壤结皮的本氏针茅(STBU+BSCs)和种植了生物土壤结皮的柠条锦鸡儿(CAKO+BSCs)设立了12个4米×2米的样地和六种处理(每种处理两个样地)。在2010年整个雨季(6月至9月)测量了3米深度内的径流、土壤流失和土壤湿度。结果表明,与裸地相比,生物土壤结皮显著减少了37.3%的径流和81.0%的土壤流失,并增加了12.4%的入渗。然而,当与本氏针茅或柠条锦鸡儿结合时,生物土壤结皮对侵蚀控制的贡献微不足道(径流减少7.4%和5.7%,土壤流失减少0.7%和0.3%)。总体而言,植被样地的上层土壤湿度低于裸地样地,尽管伴随着较高的入渗量,但当植被与生物土壤结皮结合时,这种土壤水分消耗现象更为明显。由于生物土壤结皮对侵蚀控制的贡献微不足道以及剩余加剧的土壤水分消耗,在植被覆盖度足够的样地中应考虑对生物土壤结皮进行适度干扰,以提高土壤湿度水平而不显著增加侵蚀,这被认为是必要且可行的。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66ac/4439065/09600db17100/pone.0127394.g001.jpg

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