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放牧管理对中国北方半干旱草地优先水流和入渗模式的影响机制。

Mechanisms of grazing management impact on preferential water flow and infiltration patterns in a semi-arid grassland in northern China.

机构信息

College of Desert Control Science and Engineering, Inner Mongolia Agricultural University, Hohhot 010018, China.

College of Desert Control Science and Engineering, Inner Mongolia Agricultural University, Hohhot 010018, China.

出版信息

Sci Total Environ. 2022 Mar 20;813:152082. doi: 10.1016/j.scitotenv.2021.152082. Epub 2021 Nov 30.

Abstract

Grazing management is widely used to control grassland degradation in Inner Mongolia. However, the correlation between the soil physical properties, root traits, and infiltration patterns of different types of grazing management has seldom been studied. To reveal the effect of grazing management on water infiltration and preferential flow behavior, we first investigated the soil and plant properties in a grazing exclusion (19 years, GE), cold-season grazing (19 years, CG), and free-grazing grassland (19 years, FG) in a semi-arid grassland in Inner Mongolia. Dye tracer infiltration was adopted to obtain the water infiltration patterns from different types of grazing management. Finally, root biomass and root morphological traits were measured in a field experiment. The results showed that the plant height, vegetation coverage, richness index, Shannon-Wiener index, soil water content, total porosity, and mean weight diameter were higher at the GE site than at the FG site, whereas soil bulk density and sand content were lower at the GE site than at the FG site (P < 0.05). In addition, the root mean diameter, specific root length, and root mass density were higher at the GE site than at the FG site. As a result, differences in these root traits and soil and vegetation properties affected the preferential water flow behavior in the three types of grassland. The preferential flow evaluation index (P) of the GE, CG, and FG sites was 0.89, 0.30, and 0.15, respectively, which indicated that more obvious preferential flow occurred at the GE site than at the CG and FG sites. These findings highlight that the long-term GE enhanced plant density and root biomass, which could potentially promote the natural restoration of soil pores and preferential water infiltration. Therefore, local governments and herders should implement GE rather than other grazing management practices to prevent grassland degradation.

摘要

放牧管理被广泛应用于控制内蒙古草原退化。然而,不同放牧管理类型的土壤物理性质、根系特征和入渗模式之间的相关性却很少被研究。为了揭示放牧管理对水分入渗和优先流行为的影响,我们首先调查了内蒙古半干旱草原上放牧禁牧区(19 年,GE)、冷季放牧区(19 年,CG)和自由放牧区(19 年,FG)的土壤和植物特性。采用示踪剂入渗法获得了不同放牧管理类型的水分入渗模式。最后,在田间试验中测量了根系生物量和根系形态特征。结果表明,GE 区的植物高度、植被盖度、丰富度指数、香农-威纳指数、土壤含水量、总孔隙度和平均重量直径均高于 FG 区,而 GE 区的土壤容重和沙含量则低于 FG 区(P<0.05)。此外,GE 区的根平均直径、比根长和根质量密度均高于 FG 区。因此,这些根系特征以及土壤和植被特性的差异影响了三种草地的优先水流行为。GE、CG 和 FG 区的优先流评价指数(P)分别为 0.89、0.30 和 0.15,表明 GE 区比 CG 和 FG 区优先流更为明显。这些发现表明,长期的放牧禁牧增强了植物密度和根系生物量,这可能促进了土壤孔隙的自然恢复和优先水分入渗。因此,地方政府和牧民应该实施放牧禁牧,而不是其他放牧管理措施,以防止草原退化。

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