{"title":"石勒苏益格-荷尔斯泰因州矿质耕地土壤有机碳储量及其未来碳储量潜力","authors":"Ragna-Marleen Fey, Conrad Wiermann","doi":"10.1002/jpln.12016","DOIUrl":null,"url":null,"abstract":"<div>\n \n \n <section>\n \n <h3> Background</h3>\n \n <p>Agricultural soils have the potential for long-term carbon sequestration by building up and maintaining soil organic carbon (SOC) to mitigate climate crisis. Organic soils under grassland use are often highlighted in this regard. However, given that approximately two-thirds of Schleswig-Holstein's (SH's) (Northern Germany) agriculturally used area is classified as arable land, these large areas have a potential for additional carbon storage, too.</p>\n </section>\n \n <section>\n \n <h3> Aims</h3>\n \n <p>The aim is to determine the current SOC stocks of mineral arable soils in SH and derive additional carbon storage potentials based on these data to predict additional storage potentials for the main soil type groups and geological regions. Additionally, we aim to identify the most promising agricultural practices in arable farming to exploit these potentials.</p>\n </section>\n \n <section>\n \n <h3> Methods</h3>\n \n <p>Soil data from mineral arable sites in SH were compiled, and current carbon stocks were calculated at depths of 0–30 cm and 30–100 cm. A new method (the median method) to predict additional SOC storage potentials was developed. To evaluate management practices for enhancing SOC stocks and exploit the calculated storage potentials, an optimized scenario was designed.</p>\n </section>\n \n <section>\n \n <h3> Results</h3>\n \n <p>The mean calculated SOC stocks of mineral arable soils in SH are 113 t SOC ha<sup>−1</sup> (1 m) or 71 t SOC ha<sup>−1</sup> (30 cm). The additional SOC storage potential in the topsoil (30 cm) of the total area of 9.1 Mt SOC was calculated, that is, an average potential of 13 t SOC ha<sup>−1</sup>. The scenario with five promising management practices showed that the predicted storage potential of the topsoil could be utilized by 6% in 2030 and 21% in 2040. It will take until 2090 to fully exploit the calculated potential.</p>\n </section>\n \n <section>\n \n <h3> Conclusions</h3>\n \n <p>The soils in SH show slightly higher SOC stocks and lower SOC storage potentials compared to other studies. These differences are due to variations in climate and parent material (especially marshlands), as well as the inherent limitations of the median method, which is a robust but potentially underestimating approach. It can be concluded that the exploitation of the calculated storage potentials can only be achieved through a comprehensive and long-term implementation of management practices.</p>\n </section>\n </div>","PeriodicalId":16802,"journal":{"name":"Journal of Plant Nutrition and Soil Science","volume":"188 4","pages":"658-667"},"PeriodicalIF":2.8000,"publicationDate":"2025-05-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1002/jpln.12016","citationCount":"0","resultStr":"{\"title\":\"Soil Organic Carbon (SOC) Stocks of Mineral Arable Soils in Schleswig-Holstein and Their Future Carbon Storage Potential\",\"authors\":\"Ragna-Marleen Fey, Conrad Wiermann\",\"doi\":\"10.1002/jpln.12016\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div>\\n \\n \\n <section>\\n \\n <h3> Background</h3>\\n \\n <p>Agricultural soils have the potential for long-term carbon sequestration by building up and maintaining soil organic carbon (SOC) to mitigate climate crisis. Organic soils under grassland use are often highlighted in this regard. However, given that approximately two-thirds of Schleswig-Holstein's (SH's) (Northern Germany) agriculturally used area is classified as arable land, these large areas have a potential for additional carbon storage, too.</p>\\n </section>\\n \\n <section>\\n \\n <h3> Aims</h3>\\n \\n <p>The aim is to determine the current SOC stocks of mineral arable soils in SH and derive additional carbon storage potentials based on these data to predict additional storage potentials for the main soil type groups and geological regions. Additionally, we aim to identify the most promising agricultural practices in arable farming to exploit these potentials.</p>\\n </section>\\n \\n <section>\\n \\n <h3> Methods</h3>\\n \\n <p>Soil data from mineral arable sites in SH were compiled, and current carbon stocks were calculated at depths of 0–30 cm and 30–100 cm. A new method (the median method) to predict additional SOC storage potentials was developed. To evaluate management practices for enhancing SOC stocks and exploit the calculated storage potentials, an optimized scenario was designed.</p>\\n </section>\\n \\n <section>\\n \\n <h3> Results</h3>\\n \\n <p>The mean calculated SOC stocks of mineral arable soils in SH are 113 t SOC ha<sup>−1</sup> (1 m) or 71 t SOC ha<sup>−1</sup> (30 cm). The additional SOC storage potential in the topsoil (30 cm) of the total area of 9.1 Mt SOC was calculated, that is, an average potential of 13 t SOC ha<sup>−1</sup>. The scenario with five promising management practices showed that the predicted storage potential of the topsoil could be utilized by 6% in 2030 and 21% in 2040. It will take until 2090 to fully exploit the calculated potential.</p>\\n </section>\\n \\n <section>\\n \\n <h3> Conclusions</h3>\\n \\n <p>The soils in SH show slightly higher SOC stocks and lower SOC storage potentials compared to other studies. These differences are due to variations in climate and parent material (especially marshlands), as well as the inherent limitations of the median method, which is a robust but potentially underestimating approach. 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引用次数: 0
摘要
农业土壤通过积累和维持土壤有机碳(SOC)来缓解气候危机,具有长期固碳的潜力。草地利用下的有机土壤往往是这方面的重点。然而,考虑到石勒苏益格-荷尔斯泰因州(德国北部)大约三分之二的农业用地被归类为耕地,这些大片地区也有可能储存额外的碳。目的确定盐湖矿质耕地土壤当前的有机碳储量,并根据这些数据推导出额外的碳储存潜力,以预测主要土壤类型组和地质区域的额外碳储存潜力。此外,我们的目标是确定最有前途的农业实践在耕地农业开发这些潜力。方法收集湖南矿质耕地土壤资料,计算0 ~ 30 cm和30 ~ 100 cm土壤土壤碳储量。提出了一种新的预测有机碳额外储存电位的方法(中位数法)。为了评价提高土壤有机碳储量的管理措施,并利用计算出的储量潜力,设计了一个优化方案。结果盐湖矿质耕地土壤有机碳储量分别为113 t ha - 1 (1 m)和71 t ha - 1 (30 cm)。计算了总面积为9.1 Mt的表层土壤(30 cm)的额外有机碳储存潜力,即平均潜力为13 t SOC ha - 1。采用五种有前景的管理措施的情景表明,预测的表土储存潜力在2030年可以利用6%,在2040年可以利用21%。要到2090年才能充分开发计算出的潜力。结论与其他研究区相比,沙河流域土壤有机碳储量略高,但有机碳储量潜力较低。这些差异是由于气候和母质(特别是沼泽地)的变化,以及中位数方法的固有局限性,这是一种稳健但可能低估的方法。可以得出结论,只有通过全面和长期的管理实践,才能实现计算存储潜力的开发。
Soil Organic Carbon (SOC) Stocks of Mineral Arable Soils in Schleswig-Holstein and Their Future Carbon Storage Potential
Background
Agricultural soils have the potential for long-term carbon sequestration by building up and maintaining soil organic carbon (SOC) to mitigate climate crisis. Organic soils under grassland use are often highlighted in this regard. However, given that approximately two-thirds of Schleswig-Holstein's (SH's) (Northern Germany) agriculturally used area is classified as arable land, these large areas have a potential for additional carbon storage, too.
Aims
The aim is to determine the current SOC stocks of mineral arable soils in SH and derive additional carbon storage potentials based on these data to predict additional storage potentials for the main soil type groups and geological regions. Additionally, we aim to identify the most promising agricultural practices in arable farming to exploit these potentials.
Methods
Soil data from mineral arable sites in SH were compiled, and current carbon stocks were calculated at depths of 0–30 cm and 30–100 cm. A new method (the median method) to predict additional SOC storage potentials was developed. To evaluate management practices for enhancing SOC stocks and exploit the calculated storage potentials, an optimized scenario was designed.
Results
The mean calculated SOC stocks of mineral arable soils in SH are 113 t SOC ha−1 (1 m) or 71 t SOC ha−1 (30 cm). The additional SOC storage potential in the topsoil (30 cm) of the total area of 9.1 Mt SOC was calculated, that is, an average potential of 13 t SOC ha−1. The scenario with five promising management practices showed that the predicted storage potential of the topsoil could be utilized by 6% in 2030 and 21% in 2040. It will take until 2090 to fully exploit the calculated potential.
Conclusions
The soils in SH show slightly higher SOC stocks and lower SOC storage potentials compared to other studies. These differences are due to variations in climate and parent material (especially marshlands), as well as the inherent limitations of the median method, which is a robust but potentially underestimating approach. It can be concluded that the exploitation of the calculated storage potentials can only be achieved through a comprehensive and long-term implementation of management practices.
期刊介绍:
Established in 1922, the Journal of Plant Nutrition and Soil Science (JPNSS) is an international peer-reviewed journal devoted to cover the entire spectrum of plant nutrition and soil science from different scale units, e.g. agroecosystem to natural systems. With its wide scope and focus on soil-plant interactions, JPNSS is one of the leading journals on this topic. Articles in JPNSS include reviews, high-standard original papers, and short communications and represent challenging research of international significance. The Journal of Plant Nutrition and Soil Science is one of the world’s oldest journals. You can trust in a peer-reviewed journal that has been established in the plant and soil science community for almost 100 years.
Journal of Plant Nutrition and Soil Science (ISSN 1436-8730) is published in six volumes per year, by the German Societies of Plant Nutrition (DGP) and Soil Science (DBG). Furthermore, the Journal of Plant Nutrition and Soil Science (JPNSS) is a Cooperating Journal of the International Union of Soil Science (IUSS). The journal is produced by Wiley-VCH.
Topical Divisions of the Journal of Plant Nutrition and Soil Science that are receiving increasing attention are:
JPNSS – Topical Divisions
Special timely focus in interdisciplinarity:
- sustainability & critical zone science.
Soil-Plant Interactions:
- rhizosphere science & soil ecology
- pollutant cycling & plant-soil protection
- land use & climate change.
Soil Science:
- soil chemistry & soil physics
- soil biology & biogeochemistry
- soil genesis & mineralogy.
Plant Nutrition:
- plant nutritional physiology
- nutrient dynamics & soil fertility
- ecophysiological aspects of plant nutrition.