Soil macroaggregate-occluded mineral-associated organic carbon drives the response of soil organic carbon to land use change

IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Soil & Tillage Research Pub Date : 2024-08-29 DOI:10.1016/j.still.2024.106271
Zihuan Fu , Wei Hu , Mike Beare , David Baird
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Abstract

Understanding land use effects on carbon sequestration in various soil fractions is vital to mitigating climate change and restoring soil functions. The objective of this study was to explore the effects of land use on soil organic carbon (SOC) fractions in different soil types. For this purpose, we studied the effects of long-term (>20 years) land use including dryland pasture (DP), irrigated pasture (IP) and irrigated cropland (IC) on SOC in water-stable aggregates, particle-size fractions, and their coupling relations at the surface soils (0–7.5 cm) in the Canterbury Plains, New Zealand. For each land use, three typical soil types with contrasting drainage levels (i.e. well drained Lismore soil, LIS; imperfectly drained Templeton soil, TEM; and poorly drained Waterton/Temuka soil, WAT) were selected. Macroaggregate-occluded mineral-associated organic carbon (M-MAOC) contributed to the majority of the total SOC difference and drove the response of SOC to land use change. On average, M-MAOC followed an order of IP > DP > IC. The effects of land use change from DP to IP and IC on M-MAOC varied, and these variations were dependent on soil type. The relative gain in M-MAOC with change in land use from DP to IP was the greatest in the well drained LIS soil, while both the relative and absolute loss in M-MAOC following the land use change to IC was the greatest in the poorly drained WAT soil. The interactive effects of managements (e.g. irrigation and cultivation) and soil type (e.g. soil water condition) on aggregate size distribution and macroaggregate-associated C concentration were important in explaining the responses of M-MAOC to land use change. This study advances the mechanistic understanding of total SOC dynamics in response to land use (changes) in different soil types. It also highlights the potential of M-MAOC to serve as a diagnostic fraction to reflect changes in total SOC, which may have application to global warming mitigation.

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土壤大颗粒包埋矿物相关有机碳驱动土壤有机碳对土地利用变化的响应
了解土地利用对不同土壤组分固碳的影响对于减缓气候变化和恢复土壤功能至关重要。本研究旨在探索土地利用对不同土壤类型中土壤有机碳(SOC)组分的影响。为此,我们研究了新西兰坎特伯雷平原表层土壤(0-7.5 厘米)中包括旱地牧场(DP)、灌溉牧场(IP)和灌溉耕地(IC)在内的长期(>20 年)土地利用对水稳定团聚体、颗粒大小组分中的 SOC 及其耦合关系的影响。针对每种土地用途,选择了三种排水水平截然不同的典型土壤类型(即排水良好的 Lismore 土壤,LIS;排水不完全的 Templeton 土壤,TEM;排水不良的 Waterton/Temuka 土壤,WAT)。大颗粒包含的矿物相关有机碳(M-MAOC)占总 SOC 差异的大部分,并驱动着 SOC 对土地利用变化的响应。平均而言,M-MAOC 依次为 IP > DP > IC。土地利用变化从 DP 到 IP 和 IC 对 M-MAOC 的影响各不相同,这些变化取决于土壤类型。在排水良好的 LIS 土壤中,土地利用方式从 DP 转变为 IP 后,M-MAOC 的相对增益最大;而在排水不良的 WAT 土壤中,土地利用方式转变为 IC 后,M-MAOC 的相对和绝对损失都最大。管理(如灌溉和耕作)和土壤类型(如土壤水分条件)对团聚体大小分布和大团聚体相关碳浓度的交互作用,对解释 M-MAOC 对土地利用变化的响应非常重要。这项研究推进了对不同土壤类型中总有机碳动态响应土地利用(变化)的机理认识。它还强调了 M-MAOC 作为反映总 SOC 变化的诊断组分的潜力,这可能适用于减缓全球变暖。
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来源期刊
Soil & Tillage Research
Soil & Tillage Research 农林科学-土壤科学
CiteScore
13.00
自引率
6.20%
发文量
266
审稿时长
5 months
期刊介绍: Soil & Tillage Research examines the physical, chemical and biological changes in the soil caused by tillage and field traffic. Manuscripts will be considered on aspects of soil science, physics, technology, mechanization and applied engineering for a sustainable balance among productivity, environmental quality and profitability. The following are examples of suitable topics within the scope of the journal of Soil and Tillage Research: The agricultural and biosystems engineering associated with tillage (including no-tillage, reduced-tillage and direct drilling), irrigation and drainage, crops and crop rotations, fertilization, rehabilitation of mine spoils and processes used to modify soils. Soil change effects on establishment and yield of crops, growth of plants and roots, structure and erosion of soil, cycling of carbon and nutrients, greenhouse gas emissions, leaching, runoff and other processes that affect environmental quality. Characterization or modeling of tillage and field traffic responses, soil, climate, or topographic effects, soil deformation processes, tillage tools, traction devices, energy requirements, economics, surface and subsurface water quality effects, tillage effects on weed, pest and disease control, and their interactions.
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