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The misconception of soil organic carbon sequestration notion: when do we achieve climate benefit? 土壤有机碳固存概念的误区:何时实现气候效益?
IF 3.8 3区 农林科学 Q1 SOIL SCIENCE Pub Date : 2023-12-21 DOI: 10.1111/sum.13009
Tashina Petersson, Gabriele Antoniella, Maria Vincenza Chiriacò, Lucia Perugini, T. Chiti
Soil organic carbon (SOC) sequestration is a key function of natural and semi‐natural ecosystems. Restoring this property in terrestrial ecosystems has become central to the EU's climate change mitigation and adaptation strategies. However, SOC sequestration is a widely misunderstood concept. The different methodological approaches used to investigate and compare SOC stock under sustainable agricultural practices play a key role in reinforcing misconceptions about this complex process. This commentary paper aims not only to provide a clear definition of SOC sequestration, but also to interpret the results that can be obtained for SOC stock change estimation using the SOC stock difference and the pair comparison methods, as well as to identify the soil carbon‐related processes that achieve climate mitigation. SOC sequestration can be defined as the progressive increase in a site's SOC stock compared to pre‐intervention via a net depletion and transfer of atmospheric CO2 into the soil, where it is retained as soil organic matter (SOM), by plants, plant residues or other organic solids such as the material derived from the organic fraction of farming solid waste, which can be used as a fertilizer (e.g., manure, compost, biochar, digestate), and that is produced or derived from that land‐unit. To date the most appropriate way to determine if a land unit's soil is a sink or rather a source of atmospheric CO2 is to implement the SOC stock difference method, provided the non‐occurrence of carbon exchange between ecosystems.
土壤有机碳(SOC)固存是自然和半自然生态系统的一项关键功能。恢复陆地生态系统的这一特性已成为欧盟减缓和适应气候变化战略的核心。然而,SOC 固碳是一个被广泛误解的概念。用于调查和比较可持续农业实践下 SOC 储量的不同方法在加深对这一复杂过程的误解方面起到了关键作用。本评论文章不仅旨在为 SOC 固碳提供一个清晰的定义,还旨在解释使用 SOC 储量差异法和成对比较法估算 SOC 储量变化所能获得的结果,以及确定实现气候减缓的土壤碳相关过程。SOC 固碳可定义为,与干预前相比,通过大气二氧化碳的净消耗和转移到土壤中,植物、植物残体或其他有机固体(如从农业固体废弃物的有机部分中提取的物质)将其作为土壤有机质(SOM)保留在土壤中,可用作肥料(如粪肥、堆肥、生物炭、沼渣),并由该土地单元产生或衍生,从而使该地点的 SOC 储量逐步增加。迄今为止,确定一个土地单元的土壤是大气二氧化碳的汇还是源的最合适方法是采用 SOC 储量差异法,前提是生态系统之间不存在碳交换。
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引用次数: 0
Assessment of potential soil erosion in Mongolia based on the RUSLE model and RCP 8.5 scenario 基于 RUSLE 模型和 RCP 8.5 情景的蒙古潜在土壤侵蚀评估
IF 3.8 3区 农林科学 Q1 SOIL SCIENCE Pub Date : 2023-12-19 DOI: 10.1111/sum.13005
Namuun Tuvshinjargal, Munkhnasan Lamchin, Yoonji Kim, Enerel Bayarmagnai, Seong Woo Jeon
Due to its relatively high altitude and a continental climate, environmental issues related to soil erosion and land degradation more seriously affect the ecosystem and crop production in Mongolia. As detailed soil erosion and land degradation assessments have only been performed in some regions of Mongolia, the purpose of this study is to evaluate the soil vulnerability on a national scale and predict future soil erosion under climate change prior to establishing an appropriate management plan. The Revised Universal Soil Loss Equation (RUSLE) model was chosen for this study, which reflects geographic and climatic characteristics in a vast area as the Mongolian territory. We evaluated soil erosion using historical data from 1993 and 2013 and generated predictions in the near (2041‐2060) and far future (2061‐2080) periods under the RCP 8.5 scenario. The soil erosion rates were divided into six classes: very low, low, medium, high, very high and extreme. The total of 46,039 km2 of the Mongolian territory was classified as very high and extreme risk, which is predicted to increase up to 48,961 km2 and 51,769 km2, in the near and far future periods, respectively. At the national scale, most of the soil erosion appeared in bare area, as it covers more than 60% of the total area. Meanwhile, the highest soil erosion risk was expected in high mountain ranges and ecologically vulnerable regions of the Gobi Desert and steppe area. This study identifies three land cover types with high priority for management and areas that should be considered first in the sustainable national land use and soil management plans considering regional characteristics.
由于蒙古的海拔相对较高且属于大陆性气候,与土壤侵蚀和土地退化相关的环境问题对其生态系统和作物生产的影响更为严重。由于只在蒙古的部分地区进行过详细的土壤侵蚀和土地退化评估,本研究的目的是在制定适当的管理计划之前,在全国范围内评估土壤的脆弱性,并预测气候变化下未来的土壤侵蚀情况。本研究选择了 "修订的通用土壤流失方程(RUSLE)"模型,该模型反映了蒙古幅员辽阔地区的地理和气候特征。我们利用 1993 年和 2013 年的历史数据对土壤侵蚀进行了评估,并在 RCP 8.5 情景下对近期(2041-2060 年)和远期(2061-2080 年)进行了预测。土壤侵蚀率分为六个等级:极低、低、中、高、极高和极端。蒙古 46 039 平方公里的领土被划分为极高风险和极端风险,预计在近期和远期将分别增加到 48 961 平方公里和 51 769 平方公里。在全国范围内,大部分水土流失出现在裸露地区,占总面积的 60%以上。同时,高山地区、生态脆弱的戈壁滩和草原地区的水土流失风险最高。本研究确定了三种需要优先管理的土地覆被类型,以及在考虑区域特点的可持续国家土地利用和土壤管理计划中应首先考虑的区域。
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引用次数: 0
Soil health assessment of an acidic red soil agricultural area and its restoration with biochar soil conditioners 酸性红壤农业区的土壤健康评估及使用生物炭土壤改良剂对其进行修复
IF 3.8 3区 农林科学 Q1 SOIL SCIENCE Pub Date : 2023-12-13 DOI: 10.1111/sum.13002
Qiang Li, Wanting Jiang, Junxiao Lyu
In light of growing concerns regarding food security and soil health, there is increasing emphasis on the assessment of soil health and efforts to improve or maintain the soil health of cultivated land. This case study Niutian Town in Jiangxi Province in southern China, was selected as a typical red soil and a major grain-producing area. This research involves an integrated evaluation model based on Entropy weight TOPSIS and emergy analysis to assess the soil health of cultivated land. An evaluation system was developed, comprising of 31 indicators selected on the basis of resources and environments, with an emphasis on sensitive and promising microorganisms category indicators. Additionally, experiments were conducted to assess the ecological risk of soil pollution and develop novel soil conditioners. Our results indicate that Pb, Hg and Cd present a moderate ecological risk on 92.1% of the cultivated land. Furthermore, 56.8% of the cultivated land was ‘sub-healthy’ or ‘unhealthy’. Biochar was found to be a soil conditioner with good adsorption effect, with absorption rates reaching up to 99.9% and 88.3% for Pb and Cd, respectively. Additionally, g-C3N4 was added to address pesticide contamination, which showed an adsorption rate of up to 75.2% for atrazine. This work develops a targeted remediation approach based on assessment results to address regional cropland soil health issues.
鉴于对粮食安全和土壤健康的日益关注,人们越来越重视对土壤健康的评估以及改善或保持耕地土壤健康的努力。本文以中国南方江西省牛田镇为例,选取了典型红壤和粮食主产区。研究了基于熵权TOPSIS和能值分析的耕地土壤健康综合评价模型。建立了一套评价体系,包括根据资源和环境选择的31个指标,重点是敏感和有前景的微生物类别指标。此外,还进行了土壤污染生态风险评价和新型土壤调理剂开发试验。结果表明,92.1%的耕地Pb、Hg、Cd存在中度生态风险。56.8%的耕地处于“亚健康”或“不健康”状态。生物炭是一种具有良好吸附效果的土壤调理剂,对Pb和Cd的吸收率分别达到99.9%和88.3%。此外,添加g-C3N4处理农药污染,对阿特拉津的吸附率高达75.2%。这项工作根据评估结果制定了有针对性的补救方法,以解决区域农田土壤健康问题。
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引用次数: 0
Long-term soil organic carbon changes after cropland conversion to grazed grassland in Southern Sweden 瑞典南部耕地转为放牧草地后土壤有机碳的长期变化
IF 3.8 3区 农林科学 Q1 SOIL SCIENCE Pub Date : 2023-12-11 DOI: 10.1111/sum.13004
Anna Johansson, John Livsey, Daniela Guasconi, Gustaf Hugelius, Regina Lindborg, Stefano Manzoni
There is growing awareness of the potential value of agricultural land for climate change mitigation. In Sweden, cropland areas have decreased by approximately 30% over recent decades, creating opportunities for these former croplands to be managed for climate change mitigation by increasing soil organic carbon (SOC) stocks. One potential land-use change is conversion of cropland to grazed grasslands, but the long-term effect of such changes in management are not well understood, and likely varies with soil type and site-specific conditions. Through sampling of mineral and peatland soils within a 75-yr chronosequence of land converted from crop production to grazed grassland, we assessed how time since conversion, catenary position, and soil depth affected SOC storage. The SOC stocks calculated at an equivalent soil or ash mass increased through time since conversion in mineral soils at all topographic positions, at a rate of ~0.65 % yr-1. Soils at low topographic positions gained overall more carbon. Peat SOC stocks gains after conversion were large, but only marginally significant and only when calculated at an equivalent ash mass. We conclude that conversion of mineral soil to grazed grassland promotes SOC accumulation at our sites, but climate change mitigation potential would need to be evaluated through a full greenhouse gas balance.
人们越来越意识到农业用地在减缓气候变化方面的潜在价值。近几十年来,瑞典的耕地面积减少了约 30%,这为通过增加土壤有机碳(SOC)储量来管理这些前耕地以减缓气候变化创造了机会。一种潜在的土地利用变化是将耕地转为放牧草地,但这种管理变化的长期影响尚不十分清楚,而且很可能因土壤类型和具体地点条件而异。通过对从作物生产转变为放牧草地的 75 年时间序列中的矿质土壤和泥炭地土壤进行取样,我们评估了转变后的时间、导管位置和土壤深度对 SOC 储存的影响。在所有地形位置的矿质土壤中,以等效土壤或灰烬质量计算的 SOC 储量自转换以来以每年约 0.65% 的速度增加。地势较低的土壤总体上获得了更多的碳。转化后泥炭 SOC 储量的增加量很大,但只有在按等效灰分质量计算时才会略微显著。我们的结论是,在我们的研究地点,将矿质土壤转化为放牧草地可促进 SOC 的积累,但气候变化减缓潜力需要通过全面的温室气体平衡来评估。
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引用次数: 0
Zeolites synthesized from agro-industrial residues applied in agriculture: A review and future prospects 用农用工业残渣合成的沸石:综述与未来展望
IF 3.8 3区 农林科学 Q1 SOIL SCIENCE Pub Date : 2023-12-11 DOI: 10.1111/sum.13003
Juliana de Carvalho Izidoro, Denise Alves Fungaro, Eleonora Cataldo
Zeolites have been widely applied as catalysts, wastewater treatment agents, gas adsorbents, and fertilizers, among others. However, the use of natural zeolites or those synthesized from oversaturated commercial solutions are more explored commercially than the zeolites synthesized from residues. Therefore, the aim of this review is to highlight the importance of zeolites synthesized from agro-industrial residues and their use in agriculture. This review has been divided into three different sections, i.e., zeolites, agriculture applications, synthesis of zeolites from residues, and their application in plant growth. In the first section, the definition, types, and the critical properties of zeolites are explained. The second section gives a brief review of the application of zeolites in agriculture. Finally, the synthesis of zeolites from residues, such as coal ash, rice husk ash, and sugarcane ash, with special attention to renewable sources is presented. The optimization of the synthesis of zeolites from residues with the incorporation of specific nutrients necessary for the cultivation of soybeans, corn, and sugarcane (considered the most significant crops in Brazilian agriculture in terms of the planted area) can significantly contribute to the concept of circular economy at the industries and the fulfillment of Sustainable Development Objectives, especially, the number 12 (SDO – 12 - Responsible consumption and production).
沸石已被广泛用作催化剂、废水处理剂、气体吸附剂和肥料等。然而,与从残留物中合成的沸石相比,使用天然沸石或从过饱和商业溶液中合成的沸石在商业上得到了更多的开发。因此,本综述旨在强调利用农用工业残留物合成的沸石及其在农业中应用的重要性。本综述分为三个不同的部分,即沸石、农业应用、从残渣中合成沸石及其在植物生长中的应用。第一部分解释了沸石的定义、类型和关键特性。第二部分简要回顾了沸石在农业中的应用。最后,介绍了从煤灰、稻壳灰和甘蔗灰等残渣中合成沸石的方法,特别关注了可再生资源。利用残留物合成沸石并加入大豆、玉米和甘蔗(巴西农业中种植面积最大的作物)种植所需的特定养分的优化方法,可极大地促进工业循环经济概念和可持续发展目标的实现,尤其是第 12 项目标(SDO - 12 - 负责任的消费和生产)。
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引用次数: 0
Examining soil nutrient balances and stocks under different land use and management practices in contrasting agro-ecological environments 研究对比农业生态环境中不同土地利用和管理方式下的土壤养分平衡和储存情况
IF 3.8 3区 农林科学 Q1 SOIL SCIENCE Pub Date : 2023-12-10 DOI: 10.1111/sum.13000
Temesgen Mulualem, Enyew Adgo, Derege T. Meshesha, Atsushi Tsunekawa, Nigussie Haregeweyn, Mitsuru Tsubo, Kindiye Ebabu, Misganaw Walie, Birhanu Kebede, Genetu Fekadu, Simeneh Demissie, Gizachew A. Tiruneh, Mulatu L. Berihun
Agricultural sustainability and land degradation can be monitored through studying soil nutrient dynamics. This study was conducted to investigate the balance and stocks of nitrogen (N) and phosphorus (P) under major land use types and land management (LM) practices in three contrasting agro-ecological environments in Ethiopia. We employed a nutrient monitoring approach and assessed soil N and P inputs and outputs at watershed and plot scales. Field data were collected from 72 sites representative of the major land uses of the three watersheds for the watershed-scale analysis. In addition to the watershed data, 16 experimental runoff plots were established and the response of nutrient balances to improved LM practices for the major land uses, including cropland with three treatments (control, farmyard manure [FYM], and soil bund), grazing land with three treatments (control, exclosure, and FYM + exclosure), and bushland with two treatments (control and exclosure). Nutrient balances, flows, and stocks varied significantly among agro-ecological settings, land use types, and LM practices. Severe and negative N balances were found in all agro-ecological environments, with midland (-70.8) > highland (-61.7) > lowland (-50.3 kg ha−1 yr−1), whereas slightly positive P balances were found in all agro-ecosystems. As a result, the midland (4.2% yr−1) and highland (2.1% yr−1) sites had greater N depletion rates than the lowland site (1.0% yr−1). Our results also demonstrated that applied LM practices improved N balances: by 32–40% in cropland through FYM and mineral fertilizer, by 7–18% in grazing land via FYM and exclosure, and by 6–36% in degraded bushland via exclosure, implying that, implementing FYM and mineral fertilizer for cropland and implementing FYM with exclosure on non-croplands can reverse nutrient depletion in the study sites and in other areas having similar agro-ecological conditions.
通过研究土壤养分动态,可以监测农业可持续性和土地退化。本研究旨在调查埃塞俄比亚三种截然不同的农业生态环境中,在主要土地利用类型和土地管理(LM)措施下,氮(N)和磷(P)的平衡和存量。我们采用养分监测方法,在流域和地块尺度上评估土壤氮和磷的输入和输出。为进行流域尺度分析,我们从 72 个代表三个流域主要土地用途的地点收集了实地数据。除流域数据外,还建立了 16 个实验径流地块,并对主要土地用途的养分平衡对改良土地管理方法的响应进行了分析,包括耕地的三种处理方法(对照、农家肥 [FYM] 和土埂)、牧场的三种处理方法(对照、围封和农家肥 + 围封)以及灌木林的两种处理方法(对照和围封)。不同的农业生态环境、土地利用类型和土地管理方法之间的养分平衡、流量和存量差异很大。所有农业生态系统都存在严重的负氮平衡,中地(-70.8)>;高地(-61.7)>;低地(-50.3 kg ha-1 yr-1),而所有农业生态系统都存在轻微的正磷平衡。因此,中地(4.2% yr-1)和高地(2.1% yr-1)的氮耗竭率高于低地(1.0% yr-1)。我们的研究结果还表明,应用 LM 方法可以改善氮平衡:通过施用堆肥和矿物肥料,耕地的氮平衡提高了 32-40%;通过堆肥和围封,牧场的氮平衡提高了 7-18%;通过围封,退化灌木林地的氮平衡提高了 6-36%。
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引用次数: 0
Sustainable Phosphorus Recycling: A review of advanced recovery methods with a focus on hydrothermal humification technology and potential phosphorus resources in China for this method 可持续磷回收:回顾先进的回收方法,重点是水热腐化技术和中国用于该方法的潜在磷资源
IF 3.8 3区 农林科学 Q1 SOIL SCIENCE Pub Date : 2023-12-07 DOI: 10.1111/sum.13001
Chunyu Tang, Shuang Gai, Zhuqing Liu, Long Sui, Kui Cheng, Fan Yang
The management of phosphorus (P) resources is facing dual challenges mediated by human activities: the scarcity of bioavailable P in soil and the disposal of massive undeveloped P resources in waste streams. In China, large amounts of P resources remain unexploited, including crop straw (0.9 Tg/year), pig manure (1.1 Tg/year), sludges (0.2 Tg/year), feces (0.5 Tg/year), as well as outbreaking algae (0.48 Tg/yr). Traditional P recovery technologies, including precipitation, acidulation and thermochemistry technology (PAT) and enhanced biological phosphorus removal technology (EBPR), have shown limitations in P recovery from these biomass waste streams. Hydrothermal humification technology (HTH) is a promising new technology, capable of converting typical waste streams into phosphate fertilizer for green and sustainable development. We estimate that the amount of available P that HTH could potentially extract from straw, macroalgae waste and sludge totals 0.46 Tg/year. Accordingly, the consistent development of HTH for the recycling of waste P in biomass will effectively improve China's P cycle and relieve the absence of phosphate rocks sources and environment pollution.
磷(P)资源管理正面临着由人类活动引发的双重挑战:土壤中生物可利用磷的稀缺和废物流中大量未开发磷资源的弃置。在中国,大量的磷资源仍未被开发利用,其中包括农作物秸秆(0.9 吨/年)、猪粪(1.1 吨/年)、淤泥(0.2 吨/年)、粪便(0.5 吨/年)以及破壁藻类(0.48 吨/年)。传统的磷回收技术,包括沉淀、酸化和热化学技术(PAT)以及增强型生物除磷技术(EBPR),在从这些生物质废物流中回收磷方面显示出局限性。水热腐化技术(HTH)是一种前景广阔的新技术,能够将典型的废物流转化为磷肥,促进绿色可持续发展。我们估计,水热腐殖化技术有可能从秸秆、大型藻类废物和污泥中提取的可用磷总量为 0.46 吨/年。因此,持续发展 HTH,实现生物质中废弃磷的循环利用,将有效改善中国的磷循环,缓解磷矿石来源匮乏和环境污染问题。
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引用次数: 0
How does straw returning combined with nitrogen fertilizer drive N2O emission in wheat–maize rotation system 秸秆还田配施氮肥对小麦-玉米轮作系统N2O排放的影响
IF 3.8 3区 农林科学 Q1 SOIL SCIENCE Pub Date : 2023-12-01 DOI: 10.1111/sum.12988
Jiajie Song, Jinze Bai, Zhihao Zhang, Qi Yu, Guangxin Ren, Xinhui Han, Xiaojiao Wang, Chengjie Ren, Yongzhong Feng, Xing Wang
Straw returning not only improves carbon (C) and nitrogen (N) pools, but also increases soil nitrous oxide (N2O) emissions, which poses a threat to the sustainable development of agriculture. To investigate the effect of straw return combined with nitrogen fertiliser on labile C and N pools in the soil and short-term response to soil N2O emissions in wheat–maize rotation system. The consecutive field experiment was conducted from 2019 to 2021. Single factor randomized block design was used in the experiment design, with no straw returning and no fertiliser (CK), no straw returning and nitrogen fertiliser (S0N), and straw returning combined with nitrogen fertilizer (SN). The results indicated that the SN and S0N treatments significantly (P < 0.05) increased N2O emissions by 170.45% (2.43 kg N ha-1 yr-1) and 119.5% (1.70 kg N ha-1 yr-1), soil organic carbon (SOC) by 17.23% and 14.50% and soil total nitrogen (STN) by 58.50% and 31.50%, respectively. In the 2020-2021 growing season, The soil microbial biomass carbon (SMBC) content of the SN and S0N treatments were higher than those of CK in the winter wheat seedling, winter wheat jointing, winter wheat booting, summer maize seedling, and summer maize bell-mouth stages. The structural equation model (SEM) indicated that C:N and NO3--N were the major drivers that increased soil N2O emissions, but SMBN was the main driver that decreased soil N2O emissions. The SN and S0N treatments significantly increased soil N2O emissions by increasing the NO3--N content. However, compared with the CK and S0N treatments, the SN treatment mitigated soil N2O emissions by increasing the SMBN content. More importantly, compared with CK treatment, SN treatment increased annual yield by 48.41% and 34.52%, the SN treatment could effectively improve the soil C and N pools. Therefore, straw return combined with nitrogen fertiliser (SN) may be the best choice of the treatments tested for reducing greenhouse gas emissions and achieving green and sustainable development.
秸秆还田不仅改善了碳(C)和氮(N)库,而且增加了土壤氧化亚氮(N2O)排放,对农业的可持续发展构成威胁。研究秸秆还田配施氮肥对小麦-玉米轮作系统土壤碳氮活性库的影响及其对土壤N2O排放的短期响应。2019 - 2021年连续进行田间试验。试验设计采用单因素随机区组设计,秸秆不还田不施肥(CK)、秸秆不还田不施肥(S0N)、秸秆不还田不施肥(SN)。结果表明,氮化氮和氮化氮处理显著(P < 0.05)提高了N2O排放量170.45% (2.43 kg N hm -1年-1)和119.5% (1.70 kg N hm -1年-1),土壤有机碳(SOC)分别提高了17.23%和14.50%,土壤全氮(STN)分别提高了58.50%和31.50%。在2020 ~ 2021生长季,冬小麦苗期、冬小麦拔节期、冬小麦孕穗期、夏玉米苗期和夏玉米喇口期,SN和S0N处理的土壤微生物生物量碳(SMBC)含量均高于CK。结构方程模型(SEM)表明,C:N和NO3—N是增加土壤N2O排放的主要驱动因素,而SMBN是减少土壤N2O排放的主要驱动因素。SN和S0N处理通过增加NO3——N含量显著增加了土壤N2O排放。但与CK和S0N处理相比,SN处理通过增加SMBN含量来缓解土壤N2O排放。更重要的是,与CK处理相比,SN处理的年产量分别提高了48.41%和34.52%,SN处理能有效改善土壤C、N库。因此,秸秆还田配施氮肥可能是试验处理中减少温室气体排放、实现绿色可持续发展的最佳选择。
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引用次数: 0
Combined biochar and manure addition to an agricultural soil benefits fertility, microbial activity, and mitigates manure-induced CO2 emissions 混合生物炭和肥料添加到农业土壤中有利于肥力,微生物活动,并减轻肥料引起的二氧化碳排放
IF 3.8 3区 农林科学 Q1 SOIL SCIENCE Pub Date : 2023-11-28 DOI: 10.1111/sum.12997
Manhattan Lebrun, Zubda Zahid, Magdalena Bednik, Agnieszka Medynska-Juraszek, Jiřina Száková, Martin Brtnický, Jiří Holátko, Sylvain Bourgerie, Luke Beesley, Michael Pohořelý, Jan Macků, Tereza Hnátková, Lukáš Trakal
The importance of blending biochar into manure prior to its application as a soil amendment was investigated by this laboratory and field study, hypothesizing an (i) increase in soil fertility; (ii) improvement in microbial activity; and (iii) reduction in manure-induced CO2 emissions after combining amendments. Biochar was mixed with manure (50:50 V/V) and aged in field conditions for 6 months whereafter pristine biochar, manure, and manured biochar (50:50 V/V) were incorporated into an agricultural drought-prone Regosol. All treatments and soil mixtures were incubated, with laboratory measurements of CO2 emissions taken using a coupled column respirometer set up, whilst nutrient availabilities as well as enzymatic activities were also tested.
本实验室和实地研究调查了在施用前将生物炭混合到粪肥中作为土壤改良剂的重要性,并假设:(1)增加土壤肥力;(ii)微生物活性的改善;(iii)在合并修订后减少粪便引起的二氧化碳排放。将生物炭与粪肥(50:50 V/V)混合,在田间条件下陈化6个月,然后将原始生物炭、粪肥和经过肥料处理的生物炭(50:50 V/V)掺入易干旱的农业Regosol中。所有处理和土壤混合物都进行了孵育,使用安装的耦合柱呼吸计进行了二氧化碳排放的实验室测量,同时还测试了养分有效性和酶活性。
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引用次数: 0
Delineation of high-resolution soil carbon management zones using digital soil mapping: A step towards mitigating climate change in the Northeastern Himalayas, India 利用数字土壤制图划定高分辨率土壤碳管理区:印度喜马拉雅东北部缓解气候变化的一步
IF 3.8 3区 农林科学 Q1 SOIL SCIENCE Pub Date : 2023-11-27 DOI: 10.1111/sum.12995
S. K. Reza, S. Chattaraj, S. Mukhopadhyay, A. Daripa, S. Saha, S. K. Ray
Delineation of carbon management zones (CMZs) by capturing geospatial distribution of soil organic carbon (SOC) stock down the profile is an effective strategy for precision agriculture and climate change mitigation. Satellite (Landsat OLI 8), terrain (SRTM 30 m DEM), and bioclimatic (WorldClim dataset) factors were used as covariables in this digital soil mapping approach. Depth harmonization using quadratic spline method (Equal-area) were carried out prior to quantile regression forest (QRF) algorithm based modeling to estimate SOC stock at six standard soil depths (0–5, 5–15, 15–30, 30–60, 60–100 and 100–200 cm). Soil depth and SOC stock for the whole soil profile were used for the delineation of CMZs using fuzzy k-means clustering. The predicted SOC stock, varied from 14.68 to 42.35 Mg ha-1 in the top layer (0-5 cm depth), while 17.91 to 36.88, 14.15 to 34.70, 12.55 to 35.59, 10.30 to 28.52 and 7.26 to 20.16 Mg ha-1 in the depths of 5-15, 15-30, 30-60, 60-100 and 100-200 cm, respectively. The QRF algorithm performed well in predicting SOC stock with high R2, which ranged from 0.67 to 0.83 for all the soil depths. To delineate three CMZs, modified partitioning entropy and the fuzzy performance index were used. In CMZ2, there was a significant increase in SOC stock, followed by CMZ1 and CMZ3. This zone (CMZ2) was located in the central region of the study area and was mostly covered by dense forest and perennial plantations (rubber). The CMZs provided the necessary foundation for the development of site-specific carbon management techniques that can enhance ecosystem service and meet climate change mitigation goals.
通过捕获土壤有机碳(SOC)储量在剖面上的地理空间分布来划定碳管理带(CMZs)是精准农业和减缓气候变化的有效策略。该方法采用卫星(Landsat OLI 8)、地形(SRTM 30 m DEM)和生物气候(WorldClim数据集)因子作为辅助变量。在基于分位数回归森林(QRF)算法的建模之前,采用二次样条法(等面积)进行深度协调,估算了6个标准土壤深度(0-5、5-15、15-30、30-60、60-100和100-200 cm)的土壤有机碳储量。采用模糊k-均值聚类方法,利用全剖面土壤深度和有机碳储量对cmz进行了划分。土壤有机碳储量在表层(0 ~ 5 cm)为14.68 ~ 42.35 Mg ha-1,在5 ~ 15、15 ~ 30、30 ~ 60、60 ~ 100和100 ~ 200 cm分别为17.91 ~ 36.88、14.15 ~ 34.70、12.55 ~ 35.59、10.30 ~ 28.52和7.26 ~ 20.16 Mg ha-1。QRF算法预测土壤有机碳储量具有较高的R2,在各土层深度的R2范围为0.67 ~ 0.83。采用改进的划分熵和模糊性能指标来划分三个cmz。在CMZ2中,SOC储量显著增加,其次是CMZ1和CMZ3。该区域(CMZ2)位于研究区的中心区域,主要被茂密的森林和多年生人工林(橡胶)覆盖。cmz为开发特定地点的碳管理技术提供了必要的基础,这些技术可以增强生态系统服务并实现减缓气候变化的目标。
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Soil Use and Management
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