智利巴塔哥尼亚最南端湿草甸形成的微流域土壤孔隙系统功能

IF 4 2区 农林科学 Q2 SOIL SCIENCE
J. Ivelic-Sáez, P. Cisternas, J. Clunes, J. Dörner, J. L. Arumí, S. Valle, J. Valenzuela, E. Muñoz, D. Dec, R. Horn
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引用次数: 0

摘要

湿地只占地球表面的一小部分,但提供重要的生态系统服务,如水调节、碳循环和栖息地支持。巴塔哥尼亚“维加斯”是独特的湿地生态系统,其特点是地下水补给和水文动态,与周围的草原不同。这些生态系统在支持牲畜方面发挥着至关重要的作用,其饲料产量是周围草原的六倍,并储存了超过69克千克−1的有机碳。然而,土壤结构参数(如孔隙大小分布、容重)和土壤收缩行为对巴塔哥尼亚湿地土壤水分变异和生态系统功能的影响仍然知之甚少。本研究旨在评估巴塔哥尼亚南部小流域土壤的物理容量和强度参数,包括收缩特性。我们的研究结果揭示了土壤性质的显著空间变异性,在不同的地形位置上,土壤容重(BD)在0.12至1.81 Mg m−3之间。山顶和坡脚上的矿质土壤具有较高的宏观孔隙度(在5 cm深度处高达总孔隙体积的18.1%),有利于水的运动,而Vega中心的有机土壤具有较高的总孔隙度(高达88.8%),增强了水和空气的保留。有机土壤的线性拉伸系数(COLE)达到0.078,具有较高的收缩能力。这种收缩影响了多孔系统的功能,随着大孔隙的收缩,孔隙的作用在空气传导和水储存之间发生了转变。在气候变化和干旱周期增加的驱动下,这些动态可能导致土壤功能和生态系统恢复力的重大变化。加强对土壤物理状态及其对环境变化的响应的了解可以支持可持续管理战略,使当地农业受益并保护这些关键生态系统。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Soil Pore System Functionality in a Micro-Watershed Formed by Wet Meadows (Vegas) in the Southernmost Chilean Patagonia

Wetlands occupy a small percentage of the Earth's surface but provide essential ecosystem services, such as water regulation, carbon cycling and habitat support. Patagonian “Vegas” are unique wetland ecosystems characterised by their groundwater recharge and hydrological dynamics, distinct from the surrounding steppe. These ecosystems play a critical role in supporting livestock with up to six times the forage productivity of the surrounding steppe and in storing over 69 g kg−1 of organic carbon. However, the influence of soil structure parameters (e.g., pore size distribution, bulk density) and soil shrinkage behaviour on soil moisture variability and ecosystem functions in Patagonian wetlands remains poorly understood. This study aimed to assess the physical capacity and intensity parameters of soils, including shrinkage properties, within a micro-watershed in southern Patagonia. Our findings reveal significant spatial variability in soil properties, with bulk density (BD) ranging from 0.12 to 1.81 Mg m−3 across topographic positions. Mineral soils on summits and footslopes exhibited high macroporosity (up to 18.1% of total pore volume at 5 cm depth), which facilitates water movement, while organic soils in the Vega centre had a higher total porosity (up to 88.8%) that enhances water and air retention. The coefficient of linear extensibility (COLE) for organic soils reached a level of 0.078, indicating a high shrinkage capacity. This shrinkage influenced the functionality of the porous system, shifting pore roles between air conduction and water storage as larger pores contracted. These dynamics, driven by climate change and increased drying cycles, may lead to significant shifts in soil functionality and ecosystem resilience. Enhanced understanding of soil physical states and their response to environmental changes can support sustainable management strategies, benefiting local agriculture and preserving these critical ecosystems.

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来源期刊
European Journal of Soil Science
European Journal of Soil Science 农林科学-土壤科学
CiteScore
8.20
自引率
4.80%
发文量
117
审稿时长
5 months
期刊介绍: The EJSS is an international journal that publishes outstanding papers in soil science that advance the theoretical and mechanistic understanding of physical, chemical and biological processes and their interactions in soils acting from molecular to continental scales in natural and managed environments.
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