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N2O emissions from controlled-release and conventional N-fertilizers applied to red-yellow soil in Okinawa, Japan 日本冲绳县红黄壤控释氮肥和常规氮肥的N2O排放
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-18 DOI: 10.1016/j.still.2024.106376
W.B.M.A.C. Bandara , Kazuhito Sakai , Mitsumasa Anan , Shinya Nakamura , Hideki Setouchi , Kosuke Noborio , Takamitsu Kai , R.H.K. Rathnappriya
In Okinawa, Japan, controlled-release N fertilizers (CRFs) are promoted to reduce labor and to increase fertilizer use efficiency. However, N2O emissions from N fertilizer applied to the widely prevalent Kunigami mahji (red-yellow soil), a local soil in the region, have not been examined so far. We conducted two laboratory experiments during winter and spring to compare N2O emissions between CRF and standard fertilizer (ammonium sulfate: AS) in kunigami mahji. Two seasons were selected to explore the effects of moisture and temperature on N2O emissions in relation to N fertilization. For each experiment, three soil chambers were used, each containing 1.4 kg of soil: one served as a control, and the other two received 1 g of nitrogen from either a linear-release-type CRF with 42 % N or AS with 21 % N. Over 9 weeks, N₂O emissions from the headspace of each chamber were measured every minute for 20 min, followed by 70 min of ventilation, in a continuous 90-minute cycle repeated throughout the study. Soil moisture, soil temperature, NO, and NO3-N and NH4-N in leachate were also analyzed. In Exp A (winter), nitrification was dominant, and N2O emission from CRF (emission factor, EF, 0.4 %) was 88 % lower than that from AS (EF 3.9 %). In Exp B (spring), denitrification was dominant, and N2O emission from CRF (EF 1.9 %) was 53 % lower than that from AS (EF 4 %). The frequently lower water-filled pore space (WFPS) in Exp A than in Exp B facilitated higher NO emission from AS than from CRF. Due to the consistently high WFPS in Exp B, most of the NO3 in the soil was reduced to N2O and N2. N is more readily available in AS than in CRF, facilitating higher cumulative leaching of NH4-N from AS. However, in both experiments, AS was denitrified more than CRF, producing more N2O and resulting in lower leaching of NO3-N. Our results highlight that choosing the appropriate form of fertilizer and good management of soil moisture content can reduce N2O emissions and leaching of NO3 and NH4+.
在日本冲绳推广控释氮肥(CRFs),以减少劳动力,提高肥料利用率。然而,对该地区普遍存在的红黄土(Kunigami mahji)施用氮肥所产生的N2O排放,迄今尚未进行研究。在冬季和春季进行了两个室内试验,比较了CRF与标准肥料(硫酸铵:AS)对kunigami mahji N2O排放的影响。选取两个季节,探讨水分和温度对氮肥处理下氮氧化物排放的影响。在每个实验中,使用三个土壤室,每个室含有1.4 kg的土壤:一个作为对照,另外两个从含42 % N的线性释放型CRF或含21 % N的as中获得1 g氮。在9周内,每个室顶空的N₂O排放量每分钟测量20 min,然后进行70 min的通风,在整个研究过程中重复连续90分钟的循环。土壤湿度、土壤温度、渗滤液中NO、NO3-N和NH4-N也进行了分析。试验A(冬季)以硝化作用为主,CRF(排放因子EF, 0.4 %)的N2O排放量比AS(排放因子EF, 3.9 %)低88 %。在试验B(春季)中,反硝化作用占主导地位,CRF (EF 1.9 %)的N2O排放量比AS (EF 4 %)低53 %。实验A的充水孔隙空间(WFPS)往往低于实验B,这促使AS比CRF释放更多的NO。由于实验区B的WFPS一直很高,土壤中大部分NO3−被还原为N2O和N2。氮在AS中比在CRF中更容易获得,促进了AS中NH4-N的累积淋失。然而,在两个实验中,AS的反硝化作用都大于CRF,产生更多的N2O,导致NO3-N的浸出更低。研究结果表明,选择合适的肥料形式和良好的土壤水分管理可以减少N2O的排放和NO3−和NH4+的淋溶。
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引用次数: 0
Medium-term effects of tillage, crop rotation and crop residue management practices on selected soil physical properties in the sub-humid region of Eastern Cape, South Africa 在南非东开普省半湿润地区,耕作、作物轮作和作物残茬管理措施对选定土壤物理性质的中期影响
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-18 DOI: 10.1016/j.still.2024.106420
Cossy Shayne Nonxuba , Dimpho Elvis Elephant , Adornis Dakarai Nciizah , Alen Manyevere
The conservation agricultural effects on soil physical properties are not immediately visible and are variable but might be observed in medium to long-term studies. The objective of this study was to assess the medium-term (ten year) effect of conservation agricultural practices on selected soil physical properties in a sub-humid region of Eastern Cape, South Africa. The assessment was performed on a conservation agriculture (CA) field trial established in 2012, laid out in a randomized complete block design (RCBD) with split split-plot treatment structure consisting of 16 treatment combinations replicated into 3 blocks. The main plots, sub plots and sub sub plots were allocated to tillage (no-tillage (NT) and conventional tillage (CT)), crop rotations (maize-fallow-maize (MFM); maize-soybean-maize (MFS); maize-wheat-maize (MWM); maize-wheat-soybean (MWS)), and crop residue management practices (residue retention (R+) and residue removal (R-)), respectively. Soil samples were collected from 0 – 10, 10 – 20 and 20 – 30 cm depths in the 2023/24 cropping season. The results showed that tillage practices had a significantly greater impact on bulk density (BD), porosity (ϕ) and aggregate stability (AGS)/ stability index (SI) compared to crop rotations and residue management. Soybean rotation treatments: MFS and MWS had 3.42 % and 2.08 % lower BD values compared with MFM and MWM, respectively. This is likely due to the quick decomposition of soybean residues, indicating potential improvement in soil health and soil quality with legume inclusion in rotations. Additionally, R+ plots had 24.24 % higher gravimetric water content and 25.04 % higher volumetric water content than R- plots, due to the substantial amount of SOM returned by residue decomposition. There were no significant differences observed in Ks, which could be attributed to the nature of the particle size distribution, as water moves more easily on sandy soils. These medium-term results present continual benefits from proper implementation of CA in sustainable farming and resource conservation.
保护性农业对土壤物理性质的影响不是立即可见的,而且是可变的,但可能在中长期研究中观察到。本研究的目的是评估保护性农业做法对南非东开普省半湿润地区选定土壤物理性质的中期(十年)影响。评估是在2012年建立的保护性农业(CA)田间试验中进行的,该试验采用随机完全块设计(RCBD),采用分割块处理结构,包括16个处理组合,复制到3个块中。主样地、次样地和次次样地分配为免耕(NT)和常规耕作(CT)、玉米-休耕-玉米(MFM)轮作;maize-soybean-maize (MFS);maize-wheat-maize(微波加工);玉米-小麦-大豆(MWS))和作物残留管理措施(残留保留(R+)和残留去除(R-))。在2023/24种植季采集0 ~ 10、10 ~ 20和20 ~ 30 cm深度土壤样品。结果表明,与轮作和秸秆管理相比,耕作方式对土壤容重(BD)、孔隙度(φ)和团聚稳定性(AGS)/稳定性指数(SI)的影响显著更大。大豆轮作处理:与MFM和MWM相比,MFS和MWS的BD值分别降低了3.42 %和2.08 %。这可能是由于大豆残留物的快速分解,表明轮作中含有豆类可能改善土壤健康和土壤质量。此外,R+ 地块的重量含水量比R-地块高24.24 %,体积含水量比R-地块高25.04 %,这是由于残留物分解返回了大量的SOM。在Ks中没有观察到明显的差异,这可能归因于颗粒大小分布的性质,因为水在沙质土壤中更容易移动。这些中期结果表明,在可持续农业和资源保护方面适当实施CA将带来持续效益。
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引用次数: 0
Seasonal variations of soil functions affected by straw incorporation in croplands with different degradation degrees 不同退化程度农田秸秆还田对土壤功能影响的季节变化
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-18 DOI: 10.1016/j.still.2024.106426
Chengshu Wang , Guanghui Zhang , Shiqi Chen
The reduction of soil function in croplands is widespread over the world resulting from land degradation induced by intensified agricultural practices. Straw incorporation likely affects soil function in sloping croplands. However, the quantitative influences of incorporated straw on the seasonal dynamics of soil function in croplands with different degradation degrees are still uncertain. The objective of the study is to identify the seasonal variations of different soil functions affected by straw incorporation in different degraded croplands in the black soil region of China. The results of network analysis denoted that soil functions could be fully quantified by eight factors. They were water-stable aggregate, available nitrogen, available phosphorus, humin acid, cation exchange capacity, soil organic matter, invertase and catalase. Significant seasonal variations were observed in soil function factors of different degraded croplands under straw incorporation treatment and its control (p < 0.05). Correspondingly, soil functions exhibited significant seasonal variations in various degraded croplands (p < 0.05). Soil functions were greatly enhanced by incorporated straw. In comparison to the without straw incorporation treatment, soil functions increased by 0.8 %-47.4 % during the growing season. The promotions in soil functions by straw incorporation were closely related to land degradation degree. Compared to cropland of non-degradation, the enhancements of soil functions declined by 6.2 %-58.5 %, 6.5 %-81.7 % and 11.7 %-95.2 % in the light, moderate and strong degradation croplands, respectively. Incorporated straw stimulated crop growth by improving soil functions and the crop yield increased by 12.7 %-18.7 %. Straw incorporation enhances soil functions and crop growth via improved water-stable aggregate, soil organic matter, cation exchange capacity and humin acid of different degraded croplands. The results highlight the significance of straw incorporation in degraded croplands to ameliorate soil functions and crop growth in intensive agricultural regions.
由于集约化的农业做法引起的土地退化,耕地土壤功能的下降在世界各地普遍存在。秸秆掺入可能影响坡耕地的土壤功能。然而,秸秆还田对不同退化程度农田土壤功能季节性动态的定量影响尚不确定。本研究旨在了解中国黑土区不同退化农田秸秆还田对不同土壤功能影响的季节变化。网络分析结果表明,8个因子可以完全量化土壤的功能。它们分别是水稳性团聚体、有效氮、有效磷、人殖酸、阳离子交换量、土壤有机质、转化酶和过氧化氢酶。秸秆还田与对照不同退化农田土壤功能因子的季节差异显著(p <; 0.05)。相应的,不同退化农田土壤功能表现出显著的季节变化(p <; 0.05)。秸秆掺入后土壤功能显著增强。生长季土壤功能比不还田处理提高0.8 % ~ 47.4 %。秸秆还田对土壤功能的促进作用与土地退化程度密切相关。与未退化农田相比,轻度、中度和重度退化农田土壤功能增强率分别下降了6.2 % ~ 58.5% %、6.5 % ~ 81.7 %和11.7 % ~ 95.2% %。秸秆通过改善土壤功能促进作物生长,作物产量提高12.7 % ~ 18.7 %。秸秆还田通过改善不同退化农田的水稳性团聚体、土壤有机质、阳离子交换能力和腐殖酸,促进土壤功能和作物生长。研究结果表明,在集约化农业地区,退化农田还田秸秆对改善土壤功能和作物生长具有重要意义。
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引用次数: 0
Revisiting penetrometer models for estimating root elongation 重新审视估算根系伸长的贯入计模型
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-17 DOI: 10.1016/j.still.2024.106400
Renato Paiva de Lima , Cássio Antonio Tormena , Moacir Tuzzin de Moraes , Zigomar Menezes de Souza , Mário Monteiro Rolim , Maurício Roberto Cherubin
Mechanical impedance has been reported as a major factor reducing root elongation. Penetrometer is the main tool for diagnosing mechanical soil conditions regarding root growth; however, soil mechanics processes influence root cavity expansion, friction and adhesion at the soil-metal interface which can induce root-related measurement overestimations. Models based on penetrometers have been used to estimate root elongation and assign penetration resistance thresholds, which have been used to determine soil physical limitation for plant development. In this paper, we revisited soil mechanical aspects modeling considering root-soil and penetrometer-soil interfaces, including calculation examples. Moreover, we revisited the application of penetration resistance threshold in soil integrated physical indices for root and plant growth. Our calculations showed that friction is a major factor inducing overestimates at penetrometer-soil interfaces. However, current mathematical models enable estimating normal stress for cavity expansion by removing the effect of soil adhesion and friction, and reducing the impact of penetrometer cone tip angle on soil-metal friction. Additionally, we estimated root elongation rate for a series of plant species as a function of penetrometer resistance which could be applied to soil physical indices for estimating limit plant growth threshold.
据报道,机械阻抗是降低根系伸长的主要因素。贯入仪是诊断根系生长的土壤力学条件的主要工具;然而,土壤力学过程会影响根腔的扩张、土-金属界面处的摩擦和粘附,从而导致与根相关的测量值高估。基于贯入计的模型已被用于估计根系伸长和分配贯入阻力阈值,这些阈值已被用于确定植物发育的土壤物理限制。本文重新讨论了考虑根-土和穿透-土界面的土壤力学方面的建模,包括计算实例。此外,我们还重新探讨了渗透阻力阈值在根系和植物生长的土壤综合物理指标中的应用。我们的计算表明,摩擦是导致在穿透-土壤界面高估的主要因素。然而,目前的数学模型可以通过去除土壤黏着和摩擦的影响,减少贯入仪锥尖角对土-金属摩擦的影响来估计空腔扩张的法向应力。此外,我们估计了一系列植物物种的根伸长率作为穿透电阻的函数,可以应用于土壤物理指标,以估计植物的极限生长阈值。
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引用次数: 0
Soil salinity accumulation and groundwater degradation due to overexploitation over recent 40-year period in Yaoba Oasis, China 近40年窑坝绿洲过度开发导致的土壤盐分积累与地下水退化
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-12 DOI: 10.1016/j.still.2024.106398
Ting Lu , Pingping Luo , Jucui Wang , Yudong Lu , Aidi Huo , Liming Liu
Yaoba Oasis is a traditional tillage farmland completely dependent on irrigation with groundwater. Previous investigations (1980–2015) have revealed that over-extraction of groundwater, deterioration of water quality, and soil salinization are the primary factors limiting the development of the regional agricultural economy. This study aimed to determine the impact of human activities, specifically groundwater exploitation and agricultural irrigation, on the migration of soil salinization since 1980 in the Yaoba Oasis. Specifically, water and soil samples were collected and analyzed from 90 wells and 21 soil sites. Results indicated that the groundwater level in the oasis has steadily declined at a rate of 0.04–0.59 m per year, primarily due to groundwater overexploitation. The annual average soil salt accumulation was approximately 91.1–155.2 mg/kg. Soil salinity was strongly correlated with the hydrochemical composition, with all indicators increasing along the flow path. Irrigation infiltration resulted in salt accumulation below 20 cm, with residual salts being leached by the irrigation return water. Overall, residual salt dissolution under flood irrigation and saltwater intrusion in desert salt lakes are the main reasons for soil salt accumulation and groundwater quality deterioration. To mitigate these issues and maintain the ecological balance of desert oases, it is imperative to limit the overexploitation of groundwater and reduce the amount of irrigation, thereby preventing groundwater contamination and soil salinization.
窑坝绿洲是一个完全依靠地下水灌溉的传统耕作农田。前期调查(1980-2015)表明,地下水过度开采、水质恶化和土壤盐碱化是制约区域农业经济发展的主要因素。本研究旨在确定1980年以来人类活动,特别是地下水开采和农业灌溉对瑶坝绿洲土壤盐碱化迁移的影响。具体而言,从90口井和21个土壤点收集和分析了水和土壤样品。结果表明:绿洲地下水位以每年0.04 ~ 0.59 m的速率持续下降,主要原因是地下水过度开采。年平均土壤盐分积累量约为91.1 ~ 155.2 mg/kg。土壤盐分与水化学成分呈较强的相关关系,且各指标均沿流道增加。灌溉入渗导致盐分在20 cm以下积聚,剩余盐分被灌溉回灌水淋滤。总体而言,洪水灌溉下的残盐溶解和沙漠盐湖的盐水入侵是导致土壤盐分积累和地下水水质恶化的主要原因。为了缓解这些问题,保持沙漠绿洲的生态平衡,必须限制地下水的过度开采,减少灌溉,从而防止地下水污染和土壤盐渍化。
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引用次数: 0
Effects of long-term fertiliser application on cropland soil carbon dynamics mediated by potential shifts in microbial carbon use efficiency 长期施肥对微生物碳利用效率潜在变化介导的农田土壤碳动态的影响
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-12 DOI: 10.1016/j.still.2024.106418
Di He , Guihua Li , Zhongkui Luo , Enli Wang
Fertiliser application in agricultural ecosystems affects not only the potential carbon input (via crop biomass and/or manure) into the soil, but also a series of soil processes regulating soil organic carbon (SOC) decomposition. A detailed mechanistic understanding of how fertiliser regimes affect SOC dynamics is still needed. Here we constrained the Agricultural Production Systems sIMulator (APSIM model) to long-term (> 20 years) crop and SOC measurement data collected from four trials under contrasting climatic and edaphic conditions in China. By optimizing the three most influential model parameters for SOC dynamics, i.e., the decomposition rate constant of the slow humic pool (rd_hum), the fraction of stable (non-decomposable) pool (Finert), and microbial carbon use efficiency (CUE), we analysed their responses to fertiliser application regimes to infer potential mechanisms underpinning SOC changes. Our results revealed strong effects of fertiliser regimes and sites on CUE. Sites, fertiliser regimes and their interactions explained 67 % and 1.4 % of the variation in the derived CUE and rd_hum values, respectively. Linear mixed-effects modelling showed that soil C:N ratio together with carbon input amount as a random effect explained 90 % of the variation in optimised CUE values across sites and treatments. Such impact on CUE could partly explain the impact of fertiliser and carbon input on the priming effect. Fertilisers with more carbon input (i.e., straw or manure) increased CUE by 27 % - 57 % compared with chemical fertilisers in three of four sites. However, their impacts on rd_hum was divergent when decomposition of carbon pools was simulated with first-order processes. Our results demonstrate the significant effects of fertiliser regimes on CUE and thus SOC dynamics, highlighting the importance of site-specific calibration of the current SOC models and the need to quantify uncertainty bounds of any model simulated further SOC sequestration. This study also calls for developing a clear understanding to quantify the relationship between carbon input and CUE under different environment.
在农业生态系统中施肥不仅会影响(通过作物生物量和/或粪肥)向土壤中的潜在碳输入,还会影响一系列调节土壤有机碳(SOC)分解的土壤过程。我们仍然需要从机理上详细了解肥料制度是如何影响 SOC 动态的。在此,我们将农业生产系统模拟器(APSIM)模型与中国四个气候和土壤条件截然不同的试验中收集的长期(20 年)作物和 SOC 测量数据相结合。通过优化对 SOC 动态影响最大的三个模型参数,即缓慢腐殖质池的分解速率常数(rd_hum)、稳定(不可分解)池的比例(Finert)和微生物碳利用效率(CUE),我们分析了它们对化肥施用制度的响应,以推断 SOC 变化的潜在机制。我们的研究结果表明,施肥制度和施肥地点对碳利用效率有很大影响。在得出的 CUE 和 rd_hum 值的变化中,地点、施肥制度及其交互作用分别解释了 67% 和 1.4%。线性混合效应模型显示,土壤碳氮比和作为随机效应的碳输入量可解释不同地点和处理的优化 CUE 值之间 90% 的差异。这种对 CUE 的影响可以部分解释肥料和碳投入对引诱效应的影响。与化肥相比,在四个地点中的三个地点,碳投入较多的肥料(即秸秆或粪肥)可将 CUE 提高 27% - 57%。然而,在用一阶过程模拟碳库分解时,它们对 rd_hum 的影响是不同的。我们的研究结果表明,化肥制度对 CUE 以及 SOC 动态有重大影响,这突出表明了针对具体地点校准当前 SOC 模型的重要性,以及量化任何模拟进一步 SOC 固碳的模型的不确定性边界的必要性。这项研究还要求对不同环境下的碳输入与 CUE 之间的关系有一个清晰的量化认识。
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引用次数: 0
Nature-based accumulation of organic carbon and nitrogen in citrus orchard soil with grass coverage 草地覆盖下柑橘园土壤有机碳氮的自然积累
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-12 DOI: 10.1016/j.still.2024.106419
Ludan Chen , Yuhai Bao , Xiubin He , Jie Yang , Qiao Wu , Jiaorong Lv
Grass coverage in orchards has increasingly become a sustainable practice to improve soil quality, reduce soil erosion, increase water infiltration, and enhance biodiversity and ecosystem services. It is likely to gain further adoption as a promising nature-based measure to increase organic carbon and nitrogen storage in soil. However, there is still a lack of comprehensive global quantification regarding the accumulation and availability of soil organic carbon (SOC) and total nitrogen (STN) after grass coverage in citrus orchards. A global meta-analysis was conducted to comprehensively evaluate the effects of grass coverage on SOC and STN dynamics in citrus orchards, as well as the patterns influenced by various factors. Compared to clean tillage, the accumulation rates of SOC and STN were significantly enhanced with grass coverage, with an increase of 19.98 Mg ha⁻¹ yr⁻¹ and 2.27 Mg ha⁻¹ yr⁻¹ , respectively. The microbial biomass carbon (MBC), dissolved organic carbon (DOC) and available nitrogen (AN) exhibited significantly increases following grass coverage, with average enhancements of 13.90 %, 17.94 %, and 18.04 %, respectively. The primary factors influencing the variation in SOC and STN were identified as grass age and growth modes. When grass coverage reached or exceeded 10 years and was applied uniformly across the entire orchard (full coverage), there was a more pronounced increase in SOC and STN levels. The present study provides policymakers and orchard managers with science-based evidence to guide adaptive management practices that enhance SOC and STN stocks, improve soil conditions, and increase orchard resilience to climate change.
果园植草已逐渐成为一种可持续的做法,可改善土壤质量、减少水土流失、增加水分渗透以及提高生物多样性和生态系统服务。作为增加土壤有机碳和氮储存的一种有前途的自然措施,它很可能会被进一步采用。然而,关于柑橘园植草后土壤有机碳(SOC)和全氮(STN)的积累和可用性,目前仍缺乏全面的全球量化研究。为了全面评估覆草对柑橘园土壤有机碳(SOC)和全氮(STN)动态的影响,以及受各种因素影响的模式,我们进行了一项全球荟萃分析。与清洁耕作相比,草覆盖显著提高了 SOC 和 STN 的积累率,分别增加了 19.98 兆克/公顷-¹年-¹和 2.27 兆克/公顷-¹年-¹。草地覆盖后,微生物生物量碳(MBC)、溶解有机碳(DOC)和可利用氮(AN)明显增加,平均增幅分别为 13.90 %、17.94 % 和 18.04 %。影响 SOC 和 STN 变化的主要因素是草龄和生长模式。当草的覆盖年限达到或超过 10 年,并在整个果园均匀施用(全覆盖)时,SOC 和 STN 水平会有更明显的提高。本研究为政策制定者和果园管理者提供了科学依据,以指导适应性管理实践,从而提高 SOC 和 STN 储量、改善土壤条件并增强果园对气候变化的适应能力。
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引用次数: 0
High soil bacterial diversity increases the stability of the community under grazing and nitrogen 高的土壤细菌多样性增加了放牧和施氮条件下群落的稳定性
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-10 DOI: 10.1016/j.still.2024.106414
Muhammad Usman , Mengyuan Wang , Yang Liu , Lan Li , Xiumin Zhang , Tianhao Xiao , Fujiang Hou
Grasslands are one of the major terrestrial ecosystems facing severe degradation due to climatic changes and anthropogenic activities. In northwest China, the Typical steppe and alpine meadows are the major grasslands with diverse ecosystems. These grasslands are facing degradation due to excessive livestock grazing and nitrogen (N) deposition that can alter the overall grassland ecosystem, along with the soil bacterial communities and their role in the ecosystem. The bacterial community is vital for the sustainability of grassland ecosystems as it plays a crucial role in decomposing the dead organic matter and nutrient cycling. This study conducted a grazing and N addition experiment in alpine meadows and typical steppe. The impact of short-term N application and grazing on both grasslands' soil, plant, and bacterial communities was explored. Alpine meadows had higher bacterial richness (OTUs>2000) and diversity (Shannon index>6) than the typical steppe (OTUs<900; Shannon index<5.5) due to changes in climate and ecosystem. The alpha diversity (Shannon index) of the bacterial community was observed to increase under low grazing without N addition while adding medium N (100 kg/ha) without grazing increased the diversity. The combination of medium N (100 kg/ha) addition and low grazing resulted in the highest bacterial diversity in both grasslands. In contrast, the combination of N and high grazing decreased bacterial richness and diversity. The N addition and grazing affected the bacterial community composition in the typical steppe. The co-occurrence networks revealed that the network complexity in bacterial communities of alpine meadows was higher than that of typical steppe. The rich bacterial community and high soil nutrients in alpine meadows might have led to diverse microbial functionality, which provided stability to the bacterial network. The low nutrients and water availability in typical steppe lead to a lower bacterial richness, making the bacterial community vulnerable to the changes due to grazing and N. Climate is a significant factor in shaping the grassland ecosystem and its bacterial community. The changes in the grassland’s ecosystem due to high grazing and N deposition would highly affect the distressed microbial communities in arid and semiarid regions. Further, in-depth studies are required to understand the fate of these vulnerable grasslands and design management strategies for their protection.
草地是受气候变化和人类活动影响而面临严重退化的主要陆地生态系统之一。西北地区以典型草原和高寒草甸为主,生态系统多样。由于过度放牧牲畜和氮沉降,这些草地正面临退化,氮沉降会改变整个草地生态系统,以及土壤细菌群落及其在生态系统中的作用。细菌群落对草地生态系统的可持续性至关重要,因为它在分解死有机质和养分循环中起着至关重要的作用。本研究在高寒草甸和典型草原上进行了放牧加氮试验。探讨了短期施氮和放牧对草地土壤、植物和细菌群落的影响。高寒草甸细菌丰富度(OTUs>2000)和多样性(Shannon指数>;6)均高于典型草原(OTUs<900;由于气候和生态系统的变化,Shannon指数<;5.5)。低放牧不加氮条件下细菌群落的α多样性(Shannon指数)增加,不加氮条件下添加中氮(100 kg/ha)增加了细菌群落的多样性。中氮(100 kg/ha)加量和低放牧组合使两种草地的细菌多样性最高。氮与高放牧的组合降低了土壤细菌的丰富度和多样性。加氮和放牧对典型草原细菌群落组成有影响。共现网络表明,高寒草甸细菌群落的网络复杂性高于典型草原。高寒草甸丰富的细菌群落和丰富的土壤养分可能导致了微生物功能的多样化,从而为细菌网络提供了稳定性。典型草原的养分和水分利用率低,导致细菌丰富度较低,使细菌群落容易受到放牧和氮变化的影响。气候是影响草原生态系统及其细菌群落形成的重要因素。高放牧和氮沉降对干旱半干旱区草地生态系统的影响很大。进一步,需要深入研究这些脆弱草原的命运,并设计保护它们的管理策略。
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引用次数: 0
Rice straw management options impact soil phosphorus adsorption-desorption, kinetics and thermodynamics in rice-wheat system of north-western India 水稻秸秆管理方案对印度西北部水稻-小麦系统土壤磷吸附-解吸、动力学和热力学的影响
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-09 DOI: 10.1016/j.still.2024.106403
Sandeep Sharma, Paawan Kaur
Fluctuations in soil management practices, temperature and moisture conditions can impact adsorption-desorption and bioavailability of phosphorus (P) in agricultural soils. Therefore, this study investigates P dynamics in straw-managed soils of Punjab collected from five treatments namely (1) conventional tillage (CT) after removal of rice straw (CT-R), (2) Treatment 1 plus biochar amendment at 2 Mg ha−1 (CT+biochar), (3) zero tillage with straw retention as mulch (ZT+RM), (4) CT with straw incorporation (CT+RI) and (5) CT after rice residue burned (CT+RB) after three years from an ongoing experiment in rice-wheat cropping system. The adsorption-desorption of P followed pseudo second order kinetics (R2> 0.99) and Freundlich isotherm (R2> 0.95) for all the treatments and temperatures. Freundlich adsorption capacity (KFads) varied with the physico-chemical soil properties and ranged from 10.9 to 28.5, 14.3–32.2, 18.3–40.2, and 22.5–56.5 μg1−ng−1mLn at 15, 25, 35, and 45 ± 1°C, respectively. The sequential order of P adsorption was as follows: CT+ biochar > CT+RB > ZT+RM > CT+RI > CT-R, irrespective of temperature. Thermodynamic parameters revealed feasible, spontaneous and endothermic process indicative of physio-sorption via. hydrogen bonding as the dominant mechanism in in-situ straw managed soils. The Freundlich desorption coefficient (KFdes) ranged from 54.8 to 85.2, 39.9–60.8, 23.4–37.0, 29.6–45.7 and 19.4–36.7 μg1−ng−1mLn in CT+ biochar, CT+ RB, ZT+RM, CT+RI, CT-R, respectively at studied temperatures and was greater than adsorption in all treatments indicating hysteresis. The desorption sequence was observed as: CT-R > CT+RI > ZT+RM > CT+ RB> CT+ biochar. The greater adsorption and slower desorption of P under in-situ straw managed treatments (CT+biochar, CT+RB and ZT+RM) than CT-R and CT +RI, particularly CT+ biochar compared to CT-R will lead to more P retention in soil matrix thereby preventing eutrophication and deterioration of surface waters.
土壤管理方法、温度和湿度条件的波动会影响农业土壤中磷的吸附-解吸和生物利用度。因此,本研究调查了旁遮普省秸秆管理土壤中的磷动态,收集了五种处理,即:(1)秸秆去除后的常规耕作(CT) (CT- r),(2)处理1加2 Mg ha - 1的生物炭改良(CT+生物炭),(3)秸秆保留作为覆盖物的零耕作(ZT+RM),(4)秸秆加入的CT (CT+RI)和(5)稻渣焚烧后的CT (CT+RB)经过三年的稻麦种植系统试验。P的吸附-解吸符合准二级动力学(R2>;0.99)和Freundlich等温线(R2>;0.95)所有的处理和温度。Freundlich吸附量(KFads)随土壤理化性质的变化而变化,在15、25、35和45 ± 1°C条件下分别为10.9 ~ 28.5、14.3 ~ 32.2、18.3 ~ 40.2和22.5 ~ 56.5 μg1−ng−1mLn。P的吸附顺序为:CT+ 生物炭>; CT+RB >; ZT+RM >; CT+RI >; CT- r,与温度无关。热力学参数显示了可行的、自发的和吸热的过程,表明通过物理吸附。在原位秸秆管理土壤中,氢键是主要机制。在实验温度下,CT+ 生物炭、CT+ RB、ZT+RM、CT+RI、CT- r处理的Freundlich解吸系数(KFdes)分别为54.8 ~ 85.2、39.9 ~ 60.8、23.4 ~ 37.0、29.6 ~ 45.7和19.4 ~ 36.7 μg1−ng−1mLn,且均大于吸附。解吸顺序为:CT- r >; CT+RI >; ZT+RM >; CT+ RB>; CT+ 生物炭。秸秆原位处理(CT+生物炭、CT+RB和ZT+RM)对磷的吸附比CT- r和CT+ RI更大,解吸更慢,特别是CT+ 生物炭与CT- r相比,将导致更多的磷滞留在土壤基质中,从而防止富营养化和地表水的恶化。
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引用次数: 0
Understanding the molecular mechanisms of interactions between biochar and denitrifiers in N₂O emissions reduction: Pathway to more economical and sustainable fertilizers 了解生物炭和反硝化菌在减少二氧化碳排放中的相互作用的分子机制:通往更经济和可持续肥料的途径
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-09 DOI: 10.1016/j.still.2024.106405
Babak Minofar , Nevena Milčić , Josef Maroušek , Beata Gavurová , Anna Maroušková
Biochar application to topsoil has been repeatedly and independently reported to reduce N2O emissions, yet the underlying mechanisms remain poorly understood. This study hypothesizes that biochar enhances the stability and catalytic activity of N2O reductase enzymes in denitrifying bacteria, promoting the conversion of N2O to N2 during denitrification. Interactions between biochar and the N2O reductase enzyme (PsN2OR) from the denitrifying bacterium Pseudomonas stutzeri were investigated through molecular dynamics simulations. The obtained results firstly revealed that biochar stabilizes this periplasmic enzyme in the aqueous solution via hydrophobic and hydrophilic interactions. Specifically, π–π stacking and hydrophobic interactions reduce the thermal fluctuations of hydrophobic amino acids, lowering entropy and improving enzymatic efficiency. Additionally, biochar adsorbs N2O molecules, facilitating their delivery to the active site of the enzyme and enhancing the reaction rate. Deeper understandings of molecular interactions open new pathways in developing biochar-based fertilizers with slower, more economically and more environmentally favorable release of nutrients. This new type of fertilizers creates new opportunities for the biochar market, positioning it as a valuable tool for carbon sequestration and the mitigation of N₂O emissions.
生物炭在表土上的应用已经多次被独立报道可以减少N2O的排放,但其潜在的机制仍然知之甚少。本研究假设生物炭提高了反硝化细菌中N2O还原酶的稳定性和催化活性,促进了反硝化过程中N2O向N2的转化。通过分子动力学模拟研究了生物炭与反硝化细菌stutzeri假单胞菌N2O还原酶(PsN2OR)的相互作用。得到的结果首次揭示了生物炭通过疏水和亲水性相互作用在水溶液中稳定该酶。具体来说,π -π堆叠和疏水相互作用减少了疏水氨基酸的热波动,降低了熵,提高了酶效率。此外,生物炭吸附N2O分子,促进其传递到酶的活性位点,提高反应速率。对分子相互作用的深入理解为开发更慢、更经济、更环保的生物炭基肥料开辟了新的途径。这种新型肥料为生物炭市场创造了新的机会,将其定位为固碳和减少二氧化碳排放的宝贵工具。
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引用次数: 0
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Soil & Tillage Research
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