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Surface energy exchanges and stability conditions associated with convective intense rainfall events on the central Andes of Peru
IF 5.6 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-04-26 DOI: 10.1016/j.agrformet.2025.110570
José Luis Flores-Rojas , David A. Guizado-Vidal , Jairo Valdivia-Prado , Yamina Silva , Elver Villalobos-Puma , Luis Suárez-Salas , Zenón Mata-Adauto , Hugo Abi Karam
This study presents an in-depth analysis of precipitation patterns, surface energy balance (SEB) components, and atmospheric vertical gradients (AVG) in the Huancayo Geophysical Observatory (HYGO) situated in an agricultural region inside the Mantaro valley within the central Andes of Peru, utilizing data from January 2018 to April 2022 and climatic-scale data from 1965 to 2018. Our findings reveal distinct daily and seasonal precipitation patterns, with peak occurrences in the late afternoon and early evening hours, and a pronounced seasonal variation aligning with dry and rainy periods. Analysis of 21 intense precipitation events linked to convective activity offers crucial insights for weather forecasting and disaster preparedness. These events were identified using in situ gauge pluviometers, the MIRA-35c vertical profiler radar and GPM-IMERG rainfall products. The turbulent energy fluxes: sensible (QH) and latent (QE) were estimated using the aerodynamic flux-gradient method and the ground heat flux to the surface was estimated with the scheme of Foken and Napo. Moreover, the study evaluates the efficacy of the Advanced Regional Prediction System (ARPS) model in analyzing turbulent energy fluxes during these events. A comparison with the bulk aerodynamic method indicated underestimations and overestimations by the ARPS model in predicting QH and QE, respectively, necessitating focused calibration and updates in satellite-derived data. Key observations include significant increases in QE and horizontal momentum flux (τ) before convective precipitation events, marking them as potential precursor variables. Additionally, notable decreases in water vapor mixing ratio vertical gradient (WMVG) and Richardson number (RIN), along with increases in horizontal wind gradient (HWVG), suggest changes in surface moisture fluxes and boundary layer dynamics, crucial for convective rainfall initiation. This comprehensive analysis underscores the importance of understanding atmospheric dynamics for improved prediction and preparedness strategies in the face of climatic variability.
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引用次数: 0
The caatinga dry tropical forest: A highly efficient carbon sink in South America
IF 5.6 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-04-23 DOI: 10.1016/j.agrformet.2025.110573
Keila R. Mendes , Pablo E.S. Oliveira , José Romualdo S. Lima , Magna S.B. Moura , Eduardo S. Souza , Aldrin M. Perez-Marin , John Elton B.L. Cunha , Pedro R. Mutti , Gabriel B. Costa , Thales N. Martins de Sá , Paula A.A. Araujo , Rosaria R. Ferreira , Thiago V. Marques , Daniele T. Rodrigues , Suany Campos , Mariana M.L.V. Melo , Israel V.H. Silva , Leonardo F. Morais , Fábio S. Nascimento , Iara B. Silva , Rômulo S.C. Menezes
Seasonally Dry Tropical Forests (SDTFs) may act as considerable carbon sinks, regulating the atmospheric and terrestrial carbon storage and fluxes with implications for local, regional and global climates. In the Caatinga, an endemic Brazilian SDTF, the research on the magnitude of the CO2 sink is still incipient. To address this gap, we conducted a comprehensive analysis of observed CO2 fluxes using the Eddy Covariance technique across the Caatinga, quantifying and assessing the seasonal and interannual variations in CO2 exchange under contrasting soil and climatic conditions. In our study we estimated whether the Caatinga functioned as a net source or sink of carbon at five sites during years with varying rates of rainfall. Results showed that the dynamics of CO2 flux components varied based on the spatio-temporal distribution and magnitude of rainfall and the corresponding variations in vegetation cover. Average annual accumulated Gross Primary Productivity ranged from 1167 g C m−2 in the Crystalline area to 2018 g C m−2 in the Agreste ecotone. Average annual Net Ecosystem Exchange was -775 g C m−2 (-7.7 t C ha−1). The Caatinga exhibited higher carbon use efficiency (CUE) compared to other dry forests in arid and semi-arid regions worldwide and to South American ecosystems, including the Amazon, as documented by FLUXNET2015 eddy covariance datasets. CUE values ranged from 0.31 in the Crystalline area to 0.58 in the Agreste ecotone. These findings provide robust, measurement-based evidence that the Caatinga is a highly efficient carbon sink, substantially contributing to atmospheric CO2 absorption and mitigating the growth rate of atmospheric CO2 concentration.
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引用次数: 0
Co-regulation of climate and vegetation on seasonal and interannual variations of energy exchange over a temperate grassland
IF 5.6 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-04-22 DOI: 10.1016/j.agrformet.2025.110556
Yanbing Wang , Cuihai You , Xingru Tan , Tingting Ren , Tiancheng Su , Xingguo Han , Shiping Chen
Restoration of degraded grasslands can enhance productivity and promote carbon and water cycling, but changes in energy fluxes and the partitioning of net radiation (Rn) during restoration remain poorly understood. Clarifying the role of vegetation structural and physiological regulations of energy partitioning in semiarid grasslands is critical for advancing our understanding of ecosystem functioning during grassland restoration and its feedback to climate. In this study, we investigated the seasonal and interannual variations in energy fluxes and Rn partitioning over thirteen years (2006–2018) in a long-term fenced semiarid grassland site using eddy covariance method. Our results revealed a rapid shift from sensible heat flux (H)-dominance to latent heat flux (LE)-dominance during the early growing season, aligning with the phenological development of vegetation. This transition produced d a U-shaped seasonal pattern in the Bowen ratio (β, i.e. H/LE). During the H-dominated period, Rn alone governed LE and H. In contrast, during the LE-dominated period, vegetation exerted strong control over energy partitioning through both structural (leaf area index, LAI) and physiological (canopy conductance, gc) pathways, mediated by climatic factors. The seasonal distribution of precipitation and snowmelt-derived soil moisture, combined with gc, primarily regulated interannual variability in LE, H, and β. Notably, vegetation physiology, mediated by gc, exerted significant influence control over energy exchange at both seasonal and interannual scales. Furthermore, vegetation restoration enhanced available energy but did not significantly alter LE and H fluxes. This study highlights the substantial impact of vegetation growth on energy balance in grassland ecosystems under long-term exclosure, emphasizing the need to integrate these dynamics into future sustainable management practices.
退化草地的恢复可提高生产力并促进碳和水循环,但人们对恢复过程中能量通量和净辐射(Rn)分配的变化仍然知之甚少。阐明半干旱草地植被结构和生理对能量分配的调节作用,对于促进我们了解草地恢复过程中的生态系统功能及其对气候的反馈作用至关重要。在本研究中,我们采用涡度协方差法研究了一个长期围栏的半干旱草地13年间(2006-2018年)能量通量和Rn分配的季节和年际变化。我们的研究结果表明,在早期生长季节,显热通量(H)主导迅速转变为潜热通量(LE)主导,这与植被的物候发展相一致。这一转变使鲍温比(β,即 H/LE)呈现出 U 型季节模式。与此相反,在以 LE 为主导的时期,植被通过结构(叶面积指数,LAI)和生理(冠层传导率,gc)途径,在气候因素的介导下,对能量分配施加了强有力的控制。降水和融雪衍生的土壤水分的季节性分布与gc相结合,主要调节了LE、H和β的年际变化。此外,植被恢复提高了可用能量,但并未显著改变 LE 和 H 通量。这项研究强调了长期围封条件下植被生长对草地生态系统能量平衡的重大影响,强调了将这些动态变化纳入未来可持续管理实践的必要性。
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引用次数: 0
Exploring the climate signal in the variation of winter wheat quality records in the North China Plain
IF 5.6 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-04-22 DOI: 10.1016/j.agrformet.2025.110567
Weimo Zhou , Syed Tahir Ata-Ul-Karim , Yoichiro Kato , Hongyan Liu , Kaicun Wang
Crop quality is a critical aspect of food security, impacting end-use applications and market competitiveness. There is a well-established understanding of the impacts of climate change on crop yields, while its impacts on crop quality are often overlooked. Given the critical role of wheat in global food security and the ongoing climate change, it is essential to explore the climate drivers in shaping wheat quality. This study utilized county-level survey data encompassing eight quality indicators of wheat grain, flour, and dough during 2006–2019 acquired from 363 counties in the North China Plain, the biggest wheat-producing region in China. The complex association between variation in climate factors and wheat quality was explored using an interpretable machine learning framework. The results revealed that while technological advancements and change in cultivars have improved most quality indicators, especially for dough quality, climate variation during the entire growth period accounts for 10.7 % to 25.7 % of the variations in indicators. Water-related factors had a stronger impact on wheat quality than temperature-related factors. In irrigated zones, precipitation primarily governed test weight and falling number, whereas soil moisture played a key role in determining protein and wet gluten content. In rainfed zones, the standardized precipitation evapotranspiration index (SPEI) was the primary climatic driver of variations in test weight and falling number, while extremely high temperatures predominantly influenced protein and wet gluten content. Additionally, the SPEI exhibits interaction on most indicators with normal growing degree days (GDD). Specifically, the interactive effects between GDD and SPEI reduce dough quality under warm, dry conditions. Conversely, under warm, wet conditions, this interaction negatively impacts test weight and falling number. These findings underscore the importance of drought and the threshold effects of water availability in wheat quality prediction and adaptation, providing an overview of critical quality traits most susceptible to climate and climate extremes variations during the growing season.
作物质量是粮食安全的一个重要方面,影响着最终用途和市场竞争力。人们对气候变化对作物产量的影响已经有了充分的认识,但气候变化对作物质量的影响却往往被忽视。鉴于小麦在全球粮食安全中的关键作用以及正在发生的气候变化,有必要探讨影响小麦质量的气候驱动因素。本研究利用了华北平原(中国最大的小麦产区)363 个县 2006-2019 年期间小麦谷物、面粉和面团八项质量指标的县级调查数据。研究采用可解释的机器学习框架,探讨了气候因子变化与小麦质量之间的复杂关联。结果表明,虽然技术进步和品种变化改善了大多数质量指标,尤其是面团质量,但整个生长期的气候变异占指标变异的 10.7% 至 25.7%。与温度相关的因素相比,与水相关的因素对小麦质量的影响更大。在灌溉区,降水量主要决定了测试重量和降落数值,而土壤水分在决定蛋白质和湿面筋含量方面起着关键作用。在雨水灌溉区,标准化降水蒸散指数(SPEI)是试验重量和降落数值变化的主要气候驱动因素,而极端高温则主要影响蛋白质和湿面筋含量。此外,SPEI 与正常生长度日(GDD)在大多数指标上表现出交互作用。具体来说,在温暖干燥的条件下,GDD 和 SPEI 之间的交互作用会降低面团质量。相反,在温暖潮湿的条件下,这种交互作用会对测试重量和降落数值产生负面影响。这些发现强调了干旱和水分供应的阈值效应在小麦品质预测和适应中的重要性,概述了生长季节中最易受气候和极端气候影响的关键品质性状。
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引用次数: 0
High water demand limits carbon sink and transpiration in tall forests during extreme drought in Southwest China 高需水量限制了中国西南地区特大干旱期间高大森林的碳汇和蒸腾作用
IF 5.6 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-04-21 DOI: 10.1016/j.agrformet.2025.110565
Peipei Xu , Yichen Cao , Wei Fang , Wei He , Zuo Wang , Hua Yang , Lisheng Song
Drought-related forest mortality or dieback is increasing with climate warming. Previous studies have showed canopy height was one of the most important factors that related to forest survival and growth under drought, but the mechanism of this canopy height-dependency is still unclear. Based on standardized precipitation evapotranspiration index (SPEI) data, gross primary productivity (GPP) data and vegetation transpiration data, we use linear regression (LR) and random forest (RF) model to explored the impact of canopy height on forest carbon and water cycle in southwestern China for the 2010 extreme drought. Regardless of forest types, the results showed that the decline of GPP and transpiration were not only related to drought intensity but also depend on canopy height. Tall forest (> 30 m) would lose more GPP and transpiration than short forest (< 20 m), and the increasing drought intensities would improve this canopy height-dependency, especially under extreme drought condition (SPEI < −2). Regarding how canopy height affects forest water cycle, the canopy height has correlation with both SPEI and transpiration (p < 0.001) which mean tall forest needs more water to maintain growth. These results explore the reason why forest drought resistance distinguishing by canopy height, which may have a broad range implication in forest dynamics research and management.
{"title":"High water demand limits carbon sink and transpiration in tall forests during extreme drought in Southwest China","authors":"Peipei Xu ,&nbsp;Yichen Cao ,&nbsp;Wei Fang ,&nbsp;Wei He ,&nbsp;Zuo Wang ,&nbsp;Hua Yang ,&nbsp;Lisheng Song","doi":"10.1016/j.agrformet.2025.110565","DOIUrl":"10.1016/j.agrformet.2025.110565","url":null,"abstract":"<div><div>Drought-related forest mortality or dieback is increasing with climate warming. Previous studies have showed canopy height was one of the most important factors that related to forest survival and growth under drought, but the mechanism of this canopy height-dependency is still unclear. Based on standardized precipitation evapotranspiration index (SPEI) data, gross primary productivity (GPP) data and vegetation transpiration data, we use linear regression (LR) and random forest (RF) model to explored the impact of canopy height on forest carbon and water cycle in southwestern China for the 2010 extreme drought. Regardless of forest types, the results showed that the decline of GPP and transpiration were not only related to drought intensity but also depend on canopy height. Tall forest (&gt; 30 m) would lose more GPP and transpiration than short forest (&lt; 20 m), and the increasing drought intensities would improve this canopy height-dependency, especially under extreme drought condition (SPEI &lt; −2). Regarding how canopy height affects forest water cycle, the canopy height has correlation with both SPEI and transpiration (<em>p</em> &lt; 0.001) which mean tall forest needs more water to maintain growth. These results explore the reason why forest drought resistance distinguishing by canopy height, which may have a broad range implication in forest dynamics research and management.</div></div>","PeriodicalId":50839,"journal":{"name":"Agricultural and Forest Meteorology","volume":"369 ","pages":"Article 110565"},"PeriodicalIF":5.6,"publicationDate":"2025-04-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143854438","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Plant life form determines net ecosystem CO2 exchange in a salt marsh under precipitation changes
IF 5.6 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-04-21 DOI: 10.1016/j.agrformet.2025.110572
Zhenghao Liang , Jia Song , Xinge Li , Mingliang Zhao , Xiaojing Chu , Xiaojie Wang , Peiguang Li , Xiaoshuai Zhang , Weimin Song , Siyu Wei , Ruifeng Sun , Changsheng Jiang , Guangxuan Han
Plant life form (annuals and perennials) largely determines community response to the environment. Due to variations in photosynthesis-respiration rates, changes in life form can affect ecosystem respiration (ER) and gross primary productivity (GPP), thus altering net ecosystem CO2 exchange (NEE). Precipitation changes can alter soil moisture-salinity conditions in salt marshes, thus causing significant changes in life form and CO2 sink functions. However, the directional trend and magnitude of such changes along the precipitation gradient are unclear. To fill this knowledge gap, we conducted a field manipulation experiment in a salt marsh in the Yellow River Delta, China since 2014. After six years of simulated precipitation changes (-60 %, -40 %, +0 %, +40 % and +60 % of ambient precipitation), we implemented field monitoring of plant life form, biomass, NEE, ER, GPP and soil moisture-salinity content for three years (2020–2022). Average NEE values under different treatments ranged from -4.8 ± 0.8 to -2.0 ± 0.1 μmol m-2 s-1. We observed that precipitation changes altered plant life form by regulating soil salinity. Soil salinity increased under the precipitation reduction treatments, and annuals with lower productivity replaced perennials as the dominant species, which reduced NEE by suppressing GPP. Conversely, increased precipitation decreases salinity and favored the growth of perennials with high productivity, thus stimulating NEE. NEE showed an increasing trend along the precipitation gradient in this experiment, and the presence of perennials was the key to maintaining high NEE levels. However, species simplification resulting from ongoing increases in precipitation, coupled with a greater aboveground to belowground biomass ratio indicating greater nutrient consumption to support plant growth, may reduce ecosystem resistance and negatively impact future CO2 uptake. Our results highlight that exploring how precipitation changes affect NEE based on life form can simplify the study of ecosystems. These findings can serve as a scientific reference for ecological management.
{"title":"Plant life form determines net ecosystem CO2 exchange in a salt marsh under precipitation changes","authors":"Zhenghao Liang ,&nbsp;Jia Song ,&nbsp;Xinge Li ,&nbsp;Mingliang Zhao ,&nbsp;Xiaojing Chu ,&nbsp;Xiaojie Wang ,&nbsp;Peiguang Li ,&nbsp;Xiaoshuai Zhang ,&nbsp;Weimin Song ,&nbsp;Siyu Wei ,&nbsp;Ruifeng Sun ,&nbsp;Changsheng Jiang ,&nbsp;Guangxuan Han","doi":"10.1016/j.agrformet.2025.110572","DOIUrl":"10.1016/j.agrformet.2025.110572","url":null,"abstract":"<div><div>Plant life form (annuals and perennials) largely determines community response to the environment. Due to variations in photosynthesis-respiration rates, changes in life form can affect ecosystem respiration (ER) and gross primary productivity (GPP), thus altering net ecosystem CO<sub>2</sub> exchange (NEE). Precipitation changes can alter soil moisture-salinity conditions in salt marshes, thus causing significant changes in life form and CO<sub>2</sub> sink functions. However, the directional trend and magnitude of such changes along the precipitation gradient are unclear. To fill this knowledge gap, we conducted a field manipulation experiment in a salt marsh in the Yellow River Delta, China since 2014. After six years of simulated precipitation changes (-60 %, -40 %, +0 %, +40 % and +60 % of ambient precipitation), we implemented field monitoring of plant life form, biomass, NEE, ER, GPP and soil moisture-salinity content for three years (2020–2022). Average NEE values under different treatments ranged from -4.8 ± 0.8 to -2.0 ± 0.1 μmol m<sup>-2</sup> s<sup>-1</sup>. We observed that precipitation changes altered plant life form by regulating soil salinity. Soil salinity increased under the precipitation reduction treatments, and annuals with lower productivity replaced perennials as the dominant species, which reduced NEE by suppressing GPP. Conversely, increased precipitation decreases salinity and favored the growth of perennials with high productivity, thus stimulating NEE. NEE showed an increasing trend along the precipitation gradient in this experiment, and the presence of perennials was the key to maintaining high NEE levels. However, species simplification resulting from ongoing increases in precipitation, coupled with a greater aboveground to belowground biomass ratio indicating greater nutrient consumption to support plant growth, may reduce ecosystem resistance and negatively impact future CO<sub>2</sub> uptake. Our results highlight that exploring how precipitation changes affect NEE based on life form can simplify the study of ecosystems. These findings can serve as a scientific reference for ecological management.</div></div>","PeriodicalId":50839,"journal":{"name":"Agricultural and Forest Meteorology","volume":"369 ","pages":"Article 110572"},"PeriodicalIF":5.6,"publicationDate":"2025-04-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143854439","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Effect of biochar application on yield, soil carbon pools and greenhouse gas emission in rice fields: A global meta-analysis
IF 5.6 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-04-19 DOI: 10.1016/j.agrformet.2025.110571
Shenglin Wen , Ningbo Cui , Yaosheng Wang , Daozhi Gong , Zhihui Wang , Liwen Xing , Zongjun Wu , Yixuan Zhang
Biochar is applied worldwide as an effective tool for improving rice yield and increasing soil carbon pools while contributing to greenhouse gas emission reduction. However, there is a knowledge gap concerning the effects of biochar application on rice yield, soil carbon pools, and greenhouse gas emissions in rice fields under varying environmental conditions. Therefore, we conducted a comprehensive meta-analysis of 1827 observations from 134 studies to identify the key factors influencing rice yield, soil carbon pools, and greenhouse gas emissions, and to determine their impact pathways using structural equation modeling (SEM). Results showed that biochar application significantly increased rice yield, soil organic carbon (SOC), soil carbon to nitrogen ratio (C:N ratio), and microbial biomass carbon (MBC) by 16.0 %, 37.7 %, 31.8 %, and 16.3 %, respectively, while reducing methane (CH4) emission, nitrous oxide (N2O) emission, global warming potential (GWP), and dissolved organic carbon (DOC) by 5.2 %, 14.4 %, 8.6 %, and 2.5 %, respectively. Straw-derived biochar, produced via pyrolysis at temperatures below 450 °C with the application rate of 10 t ha−1, proved to be an effective method for improving rice yield and soil carbon pools while reducing greenhouse gas emission. The SEM analysis revealed a direct positive relationship between soil properties (soil total nitrogen, soil organic carbon and pH) and rice yield, with a standardized path coefficient of 0.158 (P < 0.01). Moreover, climate conditions (mean annual air temperature (MAT) and mean annual precipitation (MAP)) had direct positive impact on N2O emission and GWP, with standardized path coefficient of 0.28 (P < 0.01) and 0.179 (P < 0.05), respectively. Biochar application is more effective for soils with SOC <10 g kg−1 and pH >8, particularly in temperate regions with MAT >15 °C. Our findings provide valuable insights into optimizing biochar application strategies to balance trade-offs between rice yield, soil carbon pools, and greenhouse gas emissions.
生物炭作为提高水稻产量、增加土壤碳库和减少温室气体排放的有效工具,在全球范围内得到广泛应用。然而,在不同环境条件下,施用生物炭对水稻产量、土壤碳库和稻田温室气体排放的影响还存在知识空白。因此,我们对来自 134 项研究的 1827 个观测数据进行了综合荟萃分析,以确定影响水稻产量、土壤碳库和温室气体排放的关键因素,并利用结构方程建模(SEM)确定其影响途径。结果表明,施用生物炭能显著增加水稻产量、土壤有机碳(SOC)、土壤碳氮比(C:N 比)和微生物生物量碳(MBC),增幅分别为 16.0%、37.7%、31.8% 和 16.3%,同时减少甲烷(CH4)排放、氧化亚氮(N2O)排放、全球升温潜能值(GWP)和溶解有机碳(DOC),增幅分别为 5.2%、14.4%、8.6% 和 2.5%。事实证明,在 450 °C 以下的温度下热解产生的秸秆生物炭(施用量为 10 吨/公顷)是提高水稻产量和土壤碳库、减少温室气体排放的有效方法。SEM 分析表明,土壤特性(土壤全氮、土壤有机碳和 pH 值)与水稻产量之间存在直接的正相关关系,标准化路径系数为 0.158 (P < 0.01)。此外,气候条件(年平均气温 (MAT) 和年平均降水量 (MAP))对 N2O 排放量和 GWP 有直接的正向影响,标准化路径系数分别为 0.28 (P < 0.01) 和 0.179 (P < 0.05)。施用生物炭对SOC为10 g kg-1、pH值为8的土壤更有效,尤其是在MAT为15 °C的温带地区。我们的研究结果为优化生物炭施用策略以平衡水稻产量、土壤碳库和温室气体排放之间的权衡提供了宝贵的见解。
{"title":"Effect of biochar application on yield, soil carbon pools and greenhouse gas emission in rice fields: A global meta-analysis","authors":"Shenglin Wen ,&nbsp;Ningbo Cui ,&nbsp;Yaosheng Wang ,&nbsp;Daozhi Gong ,&nbsp;Zhihui Wang ,&nbsp;Liwen Xing ,&nbsp;Zongjun Wu ,&nbsp;Yixuan Zhang","doi":"10.1016/j.agrformet.2025.110571","DOIUrl":"10.1016/j.agrformet.2025.110571","url":null,"abstract":"<div><div>Biochar is applied worldwide as an effective tool for improving rice yield and increasing soil carbon pools while contributing to greenhouse gas emission reduction. However, there is a knowledge gap concerning the effects of biochar application on rice yield, soil carbon pools, and greenhouse gas emissions in rice fields under varying environmental conditions. Therefore, we conducted a comprehensive meta-analysis of 1827 observations from 134 studies to identify the key factors influencing rice yield, soil carbon pools, and greenhouse gas emissions, and to determine their impact pathways using structural equation modeling (SEM). Results showed that biochar application significantly increased rice yield, soil organic carbon (SOC), soil carbon to nitrogen ratio (C:N ratio), and microbial biomass carbon (MBC) by 16.0 %, 37.7 %, 31.8 %, and 16.3 %, respectively, while reducing methane (CH<sub>4</sub>) emission, nitrous oxide (N<sub>2</sub>O) emission, global warming potential (GWP), and dissolved organic carbon (DOC) by 5.2 %, 14.4 %, 8.6 %, and 2.5 %, respectively. Straw-derived biochar, produced via pyrolysis at temperatures below 450 °C with the application rate of 10 t ha<sup>−1</sup>, proved to be an effective method for improving rice yield and soil carbon pools while reducing greenhouse gas emission. The SEM analysis revealed a direct positive relationship between soil properties (soil total nitrogen, soil organic carbon and pH) and rice yield, with a standardized path coefficient of 0.158 (<em>P</em> &lt; 0.01). Moreover, climate conditions (mean annual air temperature (MAT) and mean annual precipitation (MAP)) had direct positive impact on N<sub>2</sub>O emission and GWP, with standardized path coefficient of 0.28 (<em>P</em> &lt; 0.01) and 0.179 (<em>P</em> &lt; 0.05), respectively. Biochar application is more effective for soils with SOC &lt;10 g kg<sup>−1</sup> and pH &gt;8, particularly in temperate regions with MAT &gt;15 °C. Our findings provide valuable insights into optimizing biochar application strategies to balance trade-offs between rice yield, soil carbon pools, and greenhouse gas emissions.</div></div>","PeriodicalId":50839,"journal":{"name":"Agricultural and Forest Meteorology","volume":"369 ","pages":"Article 110571"},"PeriodicalIF":5.6,"publicationDate":"2025-04-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143850409","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Corrigendum to “Exploring unresolved inquiries regarding the meaning of Reynolds averaging and decomposition: A review” [Agricultural and Forest Meteorology 362 (2025) 110364]
IF 5.6 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-04-19 DOI: 10.1016/j.agrformet.2025.110563
Andrew S. Kowalski , Jesús Abril-Gago
{"title":"Corrigendum to “Exploring unresolved inquiries regarding the meaning of Reynolds averaging and decomposition: A review” [Agricultural and Forest Meteorology 362 (2025) 110364]","authors":"Andrew S. Kowalski ,&nbsp;Jesús Abril-Gago","doi":"10.1016/j.agrformet.2025.110563","DOIUrl":"10.1016/j.agrformet.2025.110563","url":null,"abstract":"","PeriodicalId":50839,"journal":{"name":"Agricultural and Forest Meteorology","volume":"368 ","pages":"Article 110563"},"PeriodicalIF":5.6,"publicationDate":"2025-04-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143853634","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Deciphering the link between SIF, ANPP and RUE dynamics in perennial forage crop mixtures
IF 5.6 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-04-19 DOI: 10.1016/j.agrformet.2025.110569
J. Mattera , J.M. Romero , J.G.N. Irisarri , A.A. Grimoldi , G.B. Cordon
Remote sensing estimation of aerial net primary production (ANPP) is a key challenge in precision agriculture and environmental monitoring. The Monteith model serves as the main conceptual frameworkin pastures.Sun-induced fluorescence (SIF), closely linked to photosynthesis, is a promising candidate for ANPP estimations when radiation use efficiency (RUE) undergoes physiological changes.
Our aim was to analyze SIF´s ability to estimate ANPP and RUE in forage covers with different structural and physiological characteristics. Moreover, we aimed to determine the underlying mechanisms driving these correlations. We performed a proximal sensing experiment by generating differential forage covers (alfalfa, tall fescue, and mixtures), measured across different seasons.
Alfalfa and mixture plots have shown fairly constant RUE and fluorescence emission efficiency (SIFYield) upon APAR variations. This caused SIF to be an interesting monitor of ANPP (R2 ∼ 0.5), because of their strong link with APAR. On the other hand, tall fescue showed decreasing RUE when increasing APAR, which weakens ANPP-APAR correlation (R2 ∼ 0.38). Also, reduced escape fraction weakens SIF-APAR correlation (R2 ∼ 0.09). Consequently, the ANPP-SIF correlation disappears (R2 ∼ 0.02).
This is one of the first remote sensing studies analyzing the biomass available for harvest in a field managed according to forage agronomic criteria. Our findings support the use of SIF as a monitor of ANPP of forage crops when RUE and SIF Yield can be assumed to be constant upon APAR variations. Nevertheless, correlations may not be extrapolated between different crops; careful attention must be paid to RUE variations upon APAR.
{"title":"Deciphering the link between SIF, ANPP and RUE dynamics in perennial forage crop mixtures","authors":"J. Mattera ,&nbsp;J.M. Romero ,&nbsp;J.G.N. Irisarri ,&nbsp;A.A. Grimoldi ,&nbsp;G.B. Cordon","doi":"10.1016/j.agrformet.2025.110569","DOIUrl":"10.1016/j.agrformet.2025.110569","url":null,"abstract":"<div><div>Remote sensing estimation of aerial net primary production (ANPP) is a key challenge in precision agriculture and environmental monitoring. The Monteith model serves as the main conceptual frameworkin pastures.Sun-induced fluorescence (SIF), closely linked to photosynthesis, is a promising candidate for ANPP estimations when radiation use efficiency (RUE) undergoes physiological changes.</div><div>Our aim was to analyze SIF´s ability to estimate ANPP and RUE in forage covers with different structural and physiological characteristics. Moreover, we aimed to determine the underlying mechanisms driving these correlations. We performed a proximal sensing experiment by generating differential forage covers (alfalfa, tall fescue, and mixtures), measured across different seasons.</div><div>Alfalfa and mixture plots have shown fairly constant RUE and fluorescence emission efficiency (SIF<sub>Yield</sub>) upon APAR variations. This caused SIF to be an interesting monitor of ANPP (R<sup>2</sup> ∼ 0.5), because of their strong link with APAR. On the other hand, tall fescue showed decreasing RUE when increasing APAR, which weakens ANPP-APAR correlation (R<sup>2</sup> ∼ 0.38). Also, reduced escape fraction weakens SIF-APAR correlation (R<sup>2</sup> ∼ 0.09). Consequently, the ANPP-SIF correlation disappears (R<sup>2</sup> ∼ 0.02).</div><div>This is one of the first remote sensing studies analyzing the biomass available for harvest in a field managed according to forage agronomic criteria. Our findings support the use of SIF as a monitor of ANPP of forage crops when RUE and SIF <sub>Yield</sub> can be assumed to be constant upon APAR variations. Nevertheless, correlations may not be extrapolated between different crops; careful attention must be paid to RUE variations upon APAR.</div></div>","PeriodicalId":50839,"journal":{"name":"Agricultural and Forest Meteorology","volume":"369 ","pages":"Article 110569"},"PeriodicalIF":5.6,"publicationDate":"2025-04-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143850408","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Carbon fluxes controlled by land management and disturbances at a cluster of long-term ecosystem monitoring sites in Central Europe
IF 5.6 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-04-18 DOI: 10.1016/j.agrformet.2025.110533
Thomas Grünwald, Luise Wanner, Uwe Eichelmann, Markus Hehn, Uta Moderow, Heiko Prasse, Ronald Queck, Christian Bernhofer, Matthias Mauder
Terrestrial ecosystems play a crucial role in carbon sequestration and provide vital ecosystem services such as food, energy, and raw materials. Climate change, through rising temperatures, altered precipitation patterns, and extreme events, threatens the carbon sink potential of these ecosystems, with forests and grasslands particularly at risk. Long-term data from flux tower networks offer valuable insights into how different ecosystems respond to climate change and management interventions, helping to develop strategies to mitigate greenhouse gas emissions and maintain ecosystem resilience. In this study, we present such data from a <10 km cluster of long-term FLUXNET/ICOS sites in Central Europe, comprising an old spruce forest (DE-Tha), a young oak plantation after a cleared windthrow (DE-Hzd), a permanent grassland site (DE-Gri), and an agricultural site with a crop rotation typical for this region (DE-Kli). By analysing decades of data from these eddy covariance measurement sites, the research highlights the influence of drought, management, and land cover changes on CO2 and H2O fluxes. The interannual variability of evapotranspiration depends less on land use than the CO2 exchange. Our findings show that intact forests can act as larger carbon sinks than previously estimated. DE-Tha is a consistent carbon sink, with thinning helping to maintain the CO2 sequestration at a stable level of 350 gC m−2 a−1. In contrast, disturbances like clear cutting or windthrow can cause ecosystems to become carbon sources for several years, with recovery delayed due to soil carbon losses from increased respiration (DE-Hzd). While DE-Hzd was resilient to drought, the carbon uptake of DE-Tha was significantly reduced by around 50 % during dry years compared to wet years. Furthermore, sustainable management maintains carbon sequestration and land-use practices, such as crop selection, significantly impact net ecosystem productivity. These insights are valuable for optimizing land management strategies to enhance carbon sinks in similar regions.
{"title":"Carbon fluxes controlled by land management and disturbances at a cluster of long-term ecosystem monitoring sites in Central Europe","authors":"Thomas Grünwald,&nbsp;Luise Wanner,&nbsp;Uwe Eichelmann,&nbsp;Markus Hehn,&nbsp;Uta Moderow,&nbsp;Heiko Prasse,&nbsp;Ronald Queck,&nbsp;Christian Bernhofer,&nbsp;Matthias Mauder","doi":"10.1016/j.agrformet.2025.110533","DOIUrl":"10.1016/j.agrformet.2025.110533","url":null,"abstract":"<div><div>Terrestrial ecosystems play a crucial role in carbon sequestration and provide vital ecosystem services such as food, energy, and raw materials. Climate change, through rising temperatures, altered precipitation patterns, and extreme events, threatens the carbon sink potential of these ecosystems, with forests and grasslands particularly at risk. Long-term data from flux tower networks offer valuable insights into how different ecosystems respond to climate change and management interventions, helping to develop strategies to mitigate greenhouse gas emissions and maintain ecosystem resilience. In this study, we present such data from a &lt;10 km cluster of long-term FLUXNET/ICOS sites in Central Europe, comprising an old spruce forest (DE-Tha), a young oak plantation after a cleared windthrow (DE-Hzd), a permanent grassland site (DE-Gri), and an agricultural site with a crop rotation typical for this region (DE-Kli). By analysing decades of data from these eddy covariance measurement sites, the research highlights the influence of drought, management, and land cover changes on CO<sub>2</sub> and H<sub>2</sub>O fluxes. The interannual variability of evapotranspiration depends less on land use than the CO<sub>2</sub> exchange. Our findings show that intact forests can act as larger carbon sinks than previously estimated. DE-Tha is a consistent carbon sink, with thinning helping to maintain the CO<sub>2</sub> sequestration at a stable level of 350 gC <em>m</em><sup>−2</sup> <em>a</em><sup>−1</sup>. In contrast, disturbances like clear cutting or windthrow can cause ecosystems to become carbon sources for several years, with recovery delayed due to soil carbon losses from increased respiration (DE-Hzd). While DE-Hzd was resilient to drought, the carbon uptake of DE-Tha was significantly reduced by around 50 % during dry years compared to wet years. Furthermore, sustainable management maintains carbon sequestration and land-use practices, such as crop selection, significantly impact net ecosystem productivity. These insights are valuable for optimizing land management strategies to enhance carbon sinks in similar regions.</div></div>","PeriodicalId":50839,"journal":{"name":"Agricultural and Forest Meteorology","volume":"369 ","pages":"Article 110533"},"PeriodicalIF":5.6,"publicationDate":"2025-04-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143844727","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
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Agricultural and Forest Meteorology
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