表层土壤物理性质与稳定性:由生物结皮类型决定,由干旱驱动

Yong-Gang Li, Yun-Jie Huang, Qing Zhang, Xiaoying Rong, Ye Tao, Yong-Xing Lu, Ben-Feng Yin, Xiao-Bing Zhou, Yuan-Ming Zhang
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引用次数: 0

摘要

生物结皮的发育是影响旱地土壤防风、固沙和增强地表土壤稳定性的重要因素,干旱是改变旱地土壤稳定性的重要驱动因素。生物结皮的物理性质和结沙量是表征荒漠土壤稳定性的重要指标。生物结皮物理性质与BSQ之间的关系尚不清楚,不利于全面认识生物结皮的生态功能。以西北干旱区不同演替阶段的生物结皮为研究对象,研究了生物结皮的物理性质和BSQ。测定了不同类型生物结壳的物理性质和BSQ。分析了不同类型生物结壳的物理性质和BSQ对干旱的响应。结果表明,随着生物结壳的发育,其物理性能和BSQ显著增加。随着生物壳的发育和盖度的增加,生物壳的厚度、粗糙度、抗压强度、抗剪强度和BSQ均呈显著增加趋势。BSQ和抗压强度随厚度和粗糙度的增加而增加。不同生物结皮类型的物理性质、物理多功能性(P-SMF)和BSQ随干旱程度的增加呈现显著不同的趋势。结构方程模拟结果还显示,随着干旱程度的增加,P-SMF和BSQ的响应也不同。该研究有助于全面了解生物结皮的结构和功能,特别是对防风固沙和地表稳定性的研究。该研究为确定生物结皮的分布和地表稳定性提供了新方法和新思路,对旱地土地管理和保护具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Surface soil physical properties and stability: Determined by biological soil crust type and driven by aridity in the desert regions of Northwest China

Surface soil physical properties and stability: Determined by biological soil crust type and driven by aridity in the desert regions of Northwest China

Surface soil physical properties and stability: Determined by biological soil crust type and driven by aridity in the desert regions of Northwest China

Surface soil physical properties and stability: Determined by biological soil crust type and driven by aridity in the desert regions of Northwest China

Surface soil physical properties and stability: Determined by biological soil crust type and driven by aridity in the desert regions of Northwest China

Biological soil crusts (biocrusts) development is a fundamental factor affecting stability by wind prevention, sand fixation, and desert surface soil stability enhancement, and aridity is an important driver for altering soil stability in drylands. The physical properties of biocrusts and binding sand quantity (BSQ) are important indicators for characterizing the stability of desert soil. The relationships between biocrust physical properties and BSQ are not clear, which is not conducive to a comprehensive understanding of the ecological functions of biocrusts. The different successional stages of biocrusts in the arid region of Northwest China were selected to study their physical properties and BSQ. The physical properties and BSQ of the different types of biocrusts were measured. The responses of the physical properties and BSQ of different types of biocrusts to aridity were analyzed. The results showed that the physical properties and BSQ increased significantly with biocrust development. The thickness, roughness, compressive strength, shear strength, and BSQ of the biocrusts show a significant increasing trend with the development and increase of biocrusts and coverage. BSQ and compressive strength increased with increasing thickness and roughness. Physical properties, physical multifunctionality (P-SMF), and BSQ of different biocrust types showed significantly different trends with increasing aridity. The results of structural equation modeling also revealed that the P-SMF and BSQ had different responses with increasing aridity. This study contributes to a comprehensive understanding of biocrust structure and function, particularly for wind prevention and sand fixation, as well as surface stability. This study provides a new methodology and new ideas for determining the distribution and surface stability of biocrusts and is highly important for land management and conservation in drylands.

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