Moderate pasture intensification enhances soil organic carbon stocks in a degraded Brazilian Ferralsol

IF 6.1 1区 农林科学 Q1 SOIL SCIENCE
Lucas Raimundo Bento , João Vitor dos Santos , Steffen A. Schweizer , Carla Pereira de Morais , Milene Corso Mitsuyuki , Patrícia Perondi Anchão Oliveira , José Ricardo Macedo Pezzopane , Alberto Carlos de Campos Bernardi , Ladislau Martin-Neto
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Abstract

Sustainable intensification presents a unique opportunity to enhance carbon stocks in degraded pastures by optimizing forage production and consumption, thereby increasing soil organic matter (SOM) inputs. This study aimed to (i) compare soil carbon stocks to a depth of 1 m across various intensively managed pastures subjected to nitrogen fertilization, adjustments in animal stocking rates, and rotational grazing on a previously degraded pasture (DP) in a long-term field experiment in Brazilian Ferralsols; and (ii) evaluate changes in SOM composition. We compared irrigated pastures with a high animal stocking rate (IHS), a rainfed pasture with a high animal stocking rate (RHS), and a rainfed pasture with a moderate animal stocking rate (RMS) to improve DP. The origin of SOM was assessed using the natural abundance of 13C and its composition through the H/C atomic ratio and the aromaticity index (HLIFS) obtained by laser-induced fluorescence spectroscopy. A comparison between the degraded pasture and the adjacent native vegetation showed that unmanaged pasture reduced carbon stocks by 45 Mg C ha−1. However, intensification in degraded pasture enhanced the organic carbon stocks from 102 to 139 Mg C ha−1 for RHS and 162 Mg C ha−1 for RMS in the top 1 m. These values were comparable to those of the adjacent native forest (148 Mg C ha−1). In contrast, high intensification in IHS with irrigation and high nitrogen fertilization did not increase organic carbon stocks compared to unmanaged DP, which remained at 111 Mg C ha−1. Both RHS and RMS promoted the accumulation of aliphatic compounds, as evidenced by the high H/C atomic ratio and low HLIFS index. When comparing RHS and RMS, we observed that a moderate animal stocking rate resulted in a greater accumulation of pasture-derived carbon (52 Mg C ha−1) than a high animal stocking rate (37 Mg C ha−1) in the top 30 cm. This difference is likely due to faster pasture regrowth under moderate stocking rates, leading to increased incorporation of pasture-derived SOM. Overall, moderate pasture intensification promoted carbon sequestration (2 Mg C ha−1 year−1) compared to DP by introducing carbon derived from forage, reducing nitrogen fertilizer use, and preserving carbon from native vegetation.
可持续集约化为通过优化饲草生产和消耗提高退化草场的碳储量提供了一个独特的机会,从而增加土壤有机质(SOM)的输入。本研究的目的是:(i) 在巴西费拉尔斯(Ferralsols)的一项长期田间试验中,比较各种集约化管理的牧场在施氮肥、调整牲畜存栏率以及在先前退化的牧场(DP)上轮牧后 1 米深的土壤碳储量;(ii) 评估 SOM 组成的变化。我们比较了高牲畜存栏率(IHS)的灌溉牧场、高牲畜存栏率(RHS)的雨水灌溉牧场和中等牲畜存栏率(RMS)的雨水灌溉牧场,以改善 DP。通过激光诱导荧光光谱法获得的 13C 自然丰度和 H/C 原子比及其芳香指数(HLIFS)评估了 SOM 的来源。退化牧场与邻近原生植被的比较表明,未经管理的牧场减少了 45 兆克碳公顷-1 的碳储量。然而,在退化的牧场中,加强管理可提高顶部 1 米处的有机碳储量,RHS 从 102 兆克碳/公顷增加到 139 兆克碳/公顷,RMS 从 162 兆克碳/公顷增加到 162 兆克碳/公顷。这些数值与邻近的原生林(148 Mg C ha-1)相当。与此相反,通过灌溉和高氮施肥实现高度集约化的 IHS 与未管理的 DP 相比,并没有增加有机碳储量,有机碳储量仍为 111 Mg C ha-1。从高 H/C 原子比和低 HLIFS 指数可以看出,RHS 和 RMS 都促进了脂肪族化合物的积累。在比较 RHS 和 RMS 时,我们观察到,在顶部 30 厘米处,中等牲畜存栏率比高牲畜存栏率(37 毫克碳/公顷-1)导致更多的牧草衍生碳积累(52 毫克碳/公顷-1)。这种差异可能是由于适度放牧率下牧草重新生长较快,导致牧草衍生的 SOM 吸收增加。总体而言,与DP相比,适度的牧草集约化通过引入来自牧草的碳、减少氮肥使用量以及保留来自本地植被的碳,促进了碳固存(2 Mg C ha-1 year-1)。
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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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