了解有机耕作与传统耕作对土壤有机碳特征的影响-时间顺序研究

IF 6.6 1区 农林科学 Q1 SOIL SCIENCE
Guusje J. Koorneef , Mirjam M. Pulleman , Ron G.M. de Goede , Pierre Barré , François Baudin , Sophie Q. van Rijssel , Rob N.J. Comans
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引用次数: 0

摘要

有机农业的目标是生产高质量、有营养的食物,同时维持土壤和生态系统的健康,这依赖于生态过程。土壤有机碳(SOC)的数量和质量影响着生态系统服务基础上的许多土壤生态过程。然而,有机耕作对土壤有机碳含量尤其是有机碳质量的影响尚不清楚。因此,我们研究了有机耕作对表层土壤(0-15 cm)有机碳特征的长期影响。我们在粘土为主的土壤上取样了经过认证的有机管理商业农场(0-34年有机农业)的时间顺序,与附近的传统农场配对。在沙质土壤上建立了一个类似的时间序列(0-69年的有机耕作)。除了土壤样本,我们还收集了诸如作物轮作和施肥等土壤管理的基本信息。测量了总有机碳含量和影响有机碳的土壤性质(即pH、粉土、粘土、氧化铁和氧化铝的含量)。采用高锰酸盐可氧化碳(POXC)、岩石热分析、颗粒(POM)和矿物伴生(MAOM)有机质的粒度分异以及元素C:N分析四种不同的技术来表征有机碳质量。在粘土时间序列中,特别是对于铁氧化物含量低的土壤,我们发现有机耕作可以随着时间的推移增加总有机碳含量和不稳定有机碳组分,从而导致整体有机碳稳定性降低。我们还发现有迹象表明,管理对有机碳质量的影响取决于有机碳总含量。在沙地时间序列中,有机耕作的持续时间不影响有机碳的含量和质量,这可能是因为影响有机农业与传统农业有机碳循环的管理措施在沙地中并不明显,而是在粘土时间序列中。尽管我们有严格的农场选择标准,但环境土壤条件、农场特定做法和土地利用历史的巨大变化,对确定驱动有机农业对土壤有机碳动态变化的单个过程提出了挑战。这种变化也突出了土壤内在特性对有机碳动态的重要性,以及制定土壤特定农场管理建议的必要性。尽管存在这种复杂性,但本研究清楚地揭示了有机农业改变有机碳循环的潜力,使有机碳含量总体上更高,更具有生物可利用性,从而加强了相关的生态系统服务。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Understanding the effects of organic versus conventional farming on soil organic carbon characteristics – a chronosequence study
Organic farming aims at producing high quality, nutritious food while sustaining the health of soils and ecosystems, for which it relies on ecological processes. The amount and quality of soil organic carbon (SOC) influence many soil ecological processes that underlie ecosystem services. However, the effect of organic farming on the amount and especially the quality of SOC is not yet clear. We therefore investigated the long-term influence of organic arable farming on SOC characteristics in topsoil (0–15 cm).
We sampled a chronosequence of certified organically managed commercial farms (0–34 years of organic farming) on clay-dominated soils, paired with nearby conventional counterparts. A similar chronosequence (0–69 years of organic farming) was established on sand-dominated soils. Alongside soil samples, we collected basic information on soil management such as crop rotation and fertilization. Total SOC content and soil properties that influence SOC were measured (i.e., pH, content of silt, clay, iron oxides and aluminum oxides). Four different techniques were used to characterize SOC quality, i.e., permanganate oxidizable carbon (POXC), Rock-Eval thermal analysis, size fractionation into particulate (POM) and mineral-associated (MAOM) organic matter, and elemental C:N analysis.
In the clay chronosequence, particularly for soils with a low Fe oxide content, we found that organic farming can increase the total SOC content and labile organic carbon fractions over time, thus resulting in a lower overall SOC stability. We also found indications that the effects of management on SOC quality depend on the total SOC content. In the sand chronosequence, the duration of organic farming did not affect the content nor quality of SOC, potentially because management practices influencing SOC cycling were not distinctive for organic vs. conventional farming in the sand but were in the clay chronosequence.
Despite our strict farm selection criteria, large variations in environmental soil conditions, farm-specific practices, and land use history challenged the identification of individual processes that drive the observed changes in SOC dynamics in response to organic farming. This variation also highlighted the importance of intrinsic soil properties for SOC dynamics, and the need to develop soil-specific farm management recommendations. Despite this complexity, this study has clearly revealed the potential of organic farming to change SOC cycling towards a higher and overall more bioavailable SOC content, thus strengthening associated ecosystem services.
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来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
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