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Identification of spatiotemporal changes and driving factors of ecological drought during 1982–2024 across the mainland China 1982-2024年中国大陆生态干旱时空变化及驱动因素分析
IF 6.5 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-12-12 DOI: 10.1016/j.agwat.2025.110079
Hexin Lai , Shaofeng Yan , Shikai Gao , Ruyi Men , Fei Wang , Mengting Du , Kai Feng , Yanbin Li , Wenxian Guo , Haibo Yang
Drought caused by long-term water shortage may lead to insufficient soil moisture and a decline in groundwater, affecting plant growth and species turnover, and thereby altering the structure and function of the ecosystem. The vast majority of regions in China are facing severe ecological water shortage pressure, which poses a challenge to the health of the ecosystem and the sustainable development of the economy and society. The standardized ecological water deficit index (SEWDI) adopts the actual water consumption of vegetation to characterize the ecosystem’s water supply, and calculates the ecological water deficit (EWD) as the difference between ecological water consumption (EWC) and ecological water requirements (EWR), thereby enabling dynamic assessment of regional drought stress status. Based on the SEWDI, this study used multi-source remote sensing data to reveal the dynamic changes and driving factors of ecological drought in China from 1982 to 2024, and the following main conclusions were obtained: (1) the changing trends of ecological drought in various regions of China were different, and the drought situation has been particularly severe since 2000. Except for the Huang-Huai-Hai Plain Region (HPR) and the Middle-Lower Yangtze Plain (MYP), SEWDI showed a downward trend in the other regions, indicating that ecological drought in China generally showed an increasing trend. (2) SEWDI had two seasonal mutation points, which occurred in January 2003 (confidence interval: December 2002 to March 2003) and April 2017 (confidence interval: June 2016 to March 2018). (3) The most severe ecological drought event occurred from July 2019 to April 2020, with a duration and intensity of 10 months and 9.15, respectively. The peak of the drought occurred in February 2020 (SEWDI= –1.21). (4) From spring to winter, the mean range of the grid trend feature Zs of SEWDI was –1.12 (in winter) to 0.13 (in summer), suggesting that drought in summer showed a decreasing trend, while drought in spring, autumn and winter showed an increasing trend. (5) Under the combined influence of climate change and human activities, the three optimal variable factors driving changes in ecological drought in China were evapotranspiration, soil moisture and irrigation water. The research results aim to provide a reference for the identification of ecological drought and its driving factors, and to offer a scientific theoretical basis for China’s response to climate change and ecological environment protection.
长期缺水引起的干旱可能导致土壤水分不足,地下水减少,影响植物生长和物种周转,从而改变生态系统的结构和功能。中国绝大多数地区都面临着严重的生态缺水压力,这对生态系统的健康和经济社会的可持续发展提出了挑战。标准化生态水亏指数(SEWDI)采用植被的实际耗水量来表征生态系统的供水量,并将生态水亏(EWD)计算为生态耗水量(EWC)与生态需水量(EWR)之差,从而实现区域干旱胁迫状态的动态评价。基于SEWDI,利用多源遥感数据揭示了1982 - 2024年中国生态干旱的动态变化及其驱动因素,得出以下主要结论:(1)中国各区域生态干旱变化趋势不同,2000年以来干旱形势尤为严重;除黄淮海平原区(HPR)和长江中下游平原区(MYP)外,其余区域SEWDI均呈下降趋势,表明中国生态干旱总体呈增加趋势。(2) SEWDI有两个季节性突变点,分别发生在2003年1月(置信区间:2002年12月~ 2003年3月)和2017年4月(置信区间:2016年6月~ 2018年3月)。(3)最严重的生态干旱发生在2019年7月至2020年4月,持续时间和强度分别为10个月和9.15个月。干旱高峰出现在2020年2月(SEWDI= -1.21)。(4)春季至冬季,SEWDI网格趋势特征Zs的平均变化范围为-1.12(冬季)~ 0.13(夏季),表明夏季干旱呈减少趋势,春、秋、冬季干旱呈增加趋势。(5)在气候变化和人类活动共同影响下,驱动中国生态干旱变化的3个最优变量因子是蒸散发、土壤水分和灌溉水。研究结果旨在为识别生态干旱及其驱动因素提供参考,并为中国应对气候变化和生态环境保护提供科学的理论依据。
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引用次数: 0
Optimizing deficit irrigation for climate resilience in the wheat–maize rotation of North China Plain 华北平原小麦-玉米轮作气候适应优化亏缺灌溉
IF 6.5 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-12-12 DOI: 10.1016/j.agwat.2025.110038
Xiangyu Fan, Niels Schütze
Climate change significantly impacts agricultural production and water resources management, given crop growth’s dynamic response to weather changes and climate variables’ influence on irrigation supply and demand. Consequently, clarifying the effects of climate change on agricultural productivity and identifying adaptation strategies to support sustainable agriculture and livelihood security is essential. In this study, we assessed the effects of climate change on crop rotation management and water balance by simulating crop growth using the AquaCrop model under historical and projected climate scenarios (SSP2-4.5 and SSP5-8.5). Focusing on the winter wheat–summer maize rotation, the predominant cropping system in the North China Plain, we developed a computational framework to optimize irrigation practices and quantify the relationship between irrigation and yield across one year (i.e., corresponding to a complete hydrological cycle). Simulation results indicate that maize yields are projected to decline by approximately 10%, while wheat yields may increase slightly more than 20% due to the CO2 fertilization effect. Although increased precipitation under climate change scenarios can reduce irrigation requirements, it may also lead to decreased yield stability, i.e., significantly lower yields in unfavorable years. Looking ahead, effective water demand management strategies, such as implementing water quotas, will be critical for sustainable agricultural water use. Considering constraints on irrigation water supply, total yield, and yield stability, deficit irrigation proved to be the most reliable scheduling strategy for this crop rotation system.
考虑到作物生长对天气变化的动态响应以及气候变量对灌溉供需的影响,气候变化对农业生产和水资源管理产生了重大影响。因此,澄清气候变化对农业生产力的影响并确定适应战略以支持可持续农业和生计安全至关重要。在本研究中,我们利用AquaCrop模型在历史和预估气候情景(SSP2-4.5和SSP5-8.5)下模拟作物生长,评估了气候变化对作物轮作管理和水分平衡的影响。以华北平原的主要种植制度冬小麦-夏玉米轮作为研究对象,我们开发了一个计算框架来优化灌溉实践,并量化一年内(即对应于一个完整的水循环)灌溉与产量之间的关系。模拟结果表明,由于CO2施肥效应,玉米产量预计将下降约10%,而小麦产量可能增加略高于20%。虽然气候变化情景下降水增加可以减少灌溉需求,但也可能导致产量稳定性下降,即在不利年份产量显著下降。展望未来,有效的水需求管理战略,如实施水配额,将对可持续农业用水至关重要。考虑到灌溉水量、总产量和产量稳定性的约束,亏缺灌溉是该轮作系统最可靠的调度策略。
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引用次数: 0
Film mulching synergistically enhances water productivity and crop yield in maize-soybean intercropping 地膜覆盖可协同提高玉米-大豆间作的水分生产力和作物产量
IF 6.5 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-12-12 DOI: 10.1016/j.agwat.2025.110072
Jinwen Pang , Hongji Zhang , Ruotong Zhao , Shixiong Ren , Xiang Li , Peng Zhang , Hao Feng , Qin’ge Dong
Water scarcity and limited arable land availability constrain dryland agriculture, requiring optimized resource allocation to achieve sustainable production. Film mulching and intercropping are widely applied as solutions to water and land constraints in dryland farming, but their synergistic effects and underlying mechanisms remain poorly understood. Therefore, five treatments with different planting patterns were tested in this study: monoculture maize without mulching, monoculture maize with mulching, monoculture soybean without mulching, maize–soybean intercropping without mulching, and maize–soybean intercropping with mulching in the maize strip. The soil water dynamics, crop growth dynamics, root system characteristics and root–shoot coordination, water productivity (WPc), land equivalent ratio (LER), and economic benefits were analyzed. Intercropping with mulching enhanced the resource use efficiency and reduced the risk due to yield variability. Intercropping significantly increased the soil water storage (at 120–200 cm) at harvest, lowering the drought risk compared with monoculture. The system adapted to late-growth water stress through increases in the deep-root density in maize and optimizing the maize–soybean root–shoot ratio, while mulching conserved moisture in the topsoil (0–40 cm) early. Their synergy enhanced WPc by 4.66 % and LER was 1.46. Mulched intercropping also compensated for the yield losses under no mulching, increasing the total production by 10.65–27.75 % and economic returns by 8.10–29.07 %. Intercropping with plastic film mulching can optimize the use of soil and water resources and achieves synergies to establish a sustainable cropping system that facilitates water conservation, yield increases, and efficiency improvements in dryland farming areas.
水资源短缺和有限的可耕地限制了旱地农业,需要优化资源配置以实现可持续生产。地膜和间作被广泛应用于解决旱地农业的水和土地限制,但其协同效应和潜在机制尚不清楚。因此,本研究在玉米带试验了5种不同种植模式:单作玉米不覆盖、单作玉米不覆盖、单作大豆不覆盖、玉米-大豆不覆盖间作、玉米-大豆间作覆盖。分析了土壤水分动态、作物生长动态、根系特征及根冠协调、水分生产力、土地当量比和经济效益。间作覆盖提高了资源利用效率,降低了产量变异性带来的风险。与单作相比,间作显著增加了收获期土壤储水量(120 ~ 200 cm),降低了干旱风险。该系统通过增加玉米深根密度和优化玉米-大豆根冠比来适应生长后期的水分胁迫,而覆盖在早期保持表层土壤(0-40 cm)的水分。协同作用使WPc提高4.66 %,LER提高1.46 %。覆膜间作也弥补了不覆膜下的产量损失,使总产量提高10.65 ~ 27.75% %,经济效益提高8.10 ~ 29.07 %。地膜间作可以优化利用水土资源,实现协同增效,建立旱地农区节水增产增效的可持续种植体系。
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引用次数: 0
Soil salinity estimation based on satellite hyperspectral and synthetic aperture radar remote sensing image fusion 基于卫星高光谱与合成孔径雷达遥感影像融合的土壤盐分估算
IF 6.5 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-12-12 DOI: 10.1016/j.agwat.2025.110076
Nan Lin , Xunhu Ma , Yuanyuan Sui , Ruifei Zhu , Hanlin Liu , Menghong Wu , Ranzhe Jiang
Soil salinization poses a significant threat to agricultural sustainability. High-precision remote sensing for mapping soil salinity is crucial for effective salinity management. Hyperspectral image (HSI) serve as essential data sources for regional-scale monitoring of soil salinity. However, the spectral response to soil salinity is highly susceptible to coupling effects from other soil physical properties. Synthetic Aperture Radar (SAR) remote sensing is highly sensitive to soil physical parameters and can effectively compensate for the limitations of HSI. This study proposes an HSI and SAR image fusion method based on a multi-scale, multi-depth Wasserstein Generative Adversarial Network with Gradient Penalty (MSD-WGAN-GP) to improve soil salinity estimation accuracy. A soil salinity prediction model was developed using a convolutional neural network based on 123 soil samples collected from Northeast China. The results show that: (1) HSI and SAR fusion can significantly improve the prediction accuracy of soil salinity. Compared with the prediction of soil salinity based on HSI, the R2 and RPIQ of the model increase by 0.22 and 1.13, respectively, and the RMSE is reduced by 2.68 ds·m⁻¹ . (2) Compared with the traditional image fusion method, the MSD-WGAN-GP model demonstrates superior performance in the fusion of HSI and SAR image, achieving a peak signal-to-noise ratio of 38.39 dB and a structural similarity index of 0.88. (3) The MSD-WGAN-GP model significantly improved the correlation between soil salinity and spectra, achieving an average increase of 0.32 in the correlation coefficient per spectral band, while effectively mitigating the prediction bias introduced by soil moisture and surface roughness. This study emphasizes the significance of integrating multi-source remote sensing data to comprehensively capture the multidimensional characteristics of soil, thereby enabling more accurate estimation of soil salinity.
土壤盐碱化对农业的可持续性构成重大威胁。高精度的土壤盐分遥感测绘是有效管理土壤盐分的关键。高光谱图像是区域尺度土壤盐分监测的重要数据来源。然而,光谱对土壤盐分的响应极易受到其他土壤物理性质的耦合影响。合成孔径雷达(SAR)遥感对土壤物理参数高度敏感,可有效弥补HSI的局限性。为了提高土壤盐分的估计精度,提出了一种基于多尺度、多深度Wasserstein梯度惩罚生成对抗网络(MSD-WGAN-GP)的HSI和SAR图像融合方法。基于东北地区123个土壤样本,利用卷积神经网络建立了土壤盐分预测模型。结果表明:(1)HSI与SAR融合能显著提高土壤盐分的预测精度。与基于HSI的土壤盐度预测相比,模型的R2和RPIQ分别提高了0.22和1.13,RMSE降低了2.68 ds·m⁻¹ 。(2)与传统图像融合方法相比,MSD-WGAN-GP模型在HSI与SAR图像的融合方面表现出更优异的性能,峰值信噪比达到38.39 dB,结构相似指数为0.88。(3) MSD-WGAN-GP模型显著提高了土壤盐分与光谱的相关性,相关系数每光谱波段平均提高0.32,同时有效减轻了土壤湿度和地表粗糙度带来的预测偏差。本研究强调整合多源遥感数据对全面捕捉土壤多维特征的重要性,从而更准确地估算土壤盐分。
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引用次数: 0
Monitoring sub-canopy inundation dynamics in global croplands: An unexplored application of SWOT satellite data 监测全球农田冠层淹没动态:SWOT卫星数据的未开发应用
IF 6.5 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-12-12 DOI: 10.1016/j.agwat.2025.110075
Yongzhe Chen , Shunlin Liang , Huanjun Liu , Phuping Sucharitakul , Xuejing Leng , Husheng Fang , Wenyuan Li , Han Ma , Jianglei Xu , Yichuan Ma , Lichang Yin
Inundation dynamics within croplands, particularly paddy fields, profoundly influence irrigation water consumption, greenhouse gas emissions, and crop yields. The traditional practice of continuous flooding irrigation in paddy fields has been abandoned in many regions worldwide, contributing to reduced water consumption and methane emissions. However, regional information on paddy field irrigation/inundation regime is typically limited to coarse estimates derived from meta-analyses or government reports, as no existing method enables spatiotemporally consistent monitoring of inundation beneath crop canopies worldwide. This limitation arises from the inability of optical sensors to detect water beneath dense canopies, substantial variability of SAR backscatter coefficients across crop growth stages, and the limited availability of full-polarization SAR data. Here, we develop the first method for effective year-round cropland inundation monitoring across diverse climate zones. Our method leverages coherent power (COP) rather than water level measurements from the Ka-band Radar Interferometer (KaRIn) aboard the SWOT satellite to distinguish between non-inundated, partially-inundated, and fully-inundated fields. By systematically mitigating and controlling confounding factors that can affect COP signals, including incidence angle, vegetation water content, wind speed variability and noise, we establish COP thresholds for different inundation statuses under a variety of conditions using Gaussian Mixture Models. Validated across four globally representative regions, the method's results are consistent with ground-truth photographs (17/18 match), farmer interviews, and published literature. A comparison with the CYGNSS-based Berkeley-RWAWC dataset, which spans 37.4°S37.4°N, demonstrates a better performance of our SWOT-based method. The estimated cropland inundation dynamics can provide valuable support for improved agricultural water management worldwide.
农田(尤其是水田)的淹没动态对灌溉用水、温室气体排放和作物产量产生深远影响。世界上许多地区已经放弃了稻田连续漫灌的传统做法,这有助于减少水的消耗和甲烷的排放。然而,稻田灌溉/淹没情况的区域信息通常仅限于从元分析或政府报告中得出的粗略估计,因为没有现有的方法能够对全球作物冠层下的淹没情况进行时空一致的监测。这一限制是由于光学传感器无法探测密集冠层下的水分,作物生长阶段SAR后向散射系数的显著变化,以及全极化SAR数据的有限可用性。在这里,我们开发了第一种跨不同气候带的有效的全年农田淹没监测方法。我们的方法利用相干功率(COP)而不是SWOT卫星上ka波段雷达干涉仪(KaRIn)的水位测量来区分未淹没、部分淹没和完全淹没的区域。通过系统缓解和控制入射角、植被含水量、风速变率和噪声等影响COP信号的混杂因素,利用高斯混合模型建立了不同条件下不同淹没状态的COP阈值。在全球四个具有代表性的地区进行了验证,该方法的结果与实地照片(17/18匹配)、农民访谈和已发表的文献一致。与基于cygnss的Berkeley-RWAWC数据集(跨度为37.4°- 37.4°N)的对比表明,基于swot的方法具有更好的性能。估算的农田淹没动态可以为改善全球农业用水管理提供宝贵的支持。
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引用次数: 0
Effects of extreme climate on hydrological dynamics in dryland apple orchards: a modeling study 极端气候对旱地苹果园水文动态的影响:模拟研究
IF 6.5 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-12-12 DOI: 10.1016/j.agwat.2025.110074
Yumeng Yang , Qi Liu , Xiaodong Gao , Xiaoya Shao , Min Yang , Xining Zhao
In the past decades, extreme precipitation and drought have increased in both intensity and frequency in global drylands, threatening the sustainability of agricultural systems. To address this challenge, this study refined the process-oriented STEMMUS (simultaneous transfer of energy, mass, and momentum in unsaturated soil) model by introducing a dynamic leaf area index (LAI) development sub-module, and defined scenarios incorporating variations in precipitation amount, precipitation intensity, and temperature. These scenarios elucidate the response patterns of shallow and deep soil moisture and apple orchard evapotranspiration to climatic fluctuations. Key findings reveal that, at the interannual scale, increased growing-season precipitation significantly enhanced soil water storage in both shallow (0–200 cm) and deep (200–450 cm) layers. High-intensity precipitation partially increased soil water storage, particularly under reduced precipitation scenarios, though its contribution to deep soil remained limited. Compared to ambient temperature conditions, 2°C warming resulted in maximum reductions of 30.6 mm and 29.7 mm in shallow and deep soil water storage, respectively. Growing-season cumulative canopy transpiration (T), soil evaporation (E), and T/ET all increased significantly with greater precipitation. Conversely, high-intensity precipitation and 2°C warming reduced cumulative transpiration by 9.7–16.4 % and 7.2–18.3 %, respectively, while T/ET decreased by 4.0–9.4 % and 8.9–15.5 %. Notably, 2°C warming markedly amplified cumulative soil evaporation by 11.5–15.7 %, whereas high-intensity precipitation had no significant effect on soil evaporation. These findings provide a theoretical foundation for developing sustainable water management and climate adaptation strategies in dryland agroecosystems.
在过去几十年里,全球干旱地区极端降水和干旱的强度和频率都有所增加,威胁到农业系统的可持续性。为了解决这一挑战,本研究通过引入动态叶面积指数(LAI)发展子模块,改进了面向过程的STEMMUS(非饱和土壤中能量、质量和动量的同时转移)模型,并定义了包含降雨量、降水强度和温度变化的情景。这些情景阐明了浅层和深层土壤水分和苹果园蒸散对气候波动的响应模式。主要研究结果表明,在年际尺度上,生长季降水的增加显著提高了浅层(0-200 cm)和深层(200-450 cm)土壤储水量。高强度降水部分增加了土壤储水量,特别是在降水减少的情况下,尽管其对深层土壤的贡献仍然有限。与环境温度相比,升温2°C导致浅层和深层土壤储水量分别最大减少30.6 mm和29.7 mm。生长季累积冠层蒸腾(T)、土壤蒸发量(E)和T/ET均随降水增加而显著增加。相反,高强度降水和2°C增温分别使累积蒸腾减少9.7 ~ 16.4% %和7.2 ~ 18.3 %,而T/ET减少4.0 ~ 9.4 %和8.9 ~ 15.5 %。值得注意的是,2°C升温显著增加了土壤累计蒸发量11.5 ~ 15.7 %,而高强度降水对土壤蒸发量没有显著影响。这些发现为制定旱地农业生态系统可持续水资源管理和气候适应战略提供了理论基础。
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引用次数: 0
Corrigendum to “Micro-sprinkler irrigation with optimal irrigation regimes maintain grain yields while increasing carbon emission efficiency and water productivity of winter wheat on the North China Plain” [Agric. Water Manag. 321 (2025) 109933] 华北平原最佳灌溉制度下的微喷灌在保持粮食产量的同时提高了冬小麦的碳排放效率和水分生产力[j]。水管理。321 (2025)109933]
IF 6.5 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-12-11 DOI: 10.1016/j.agwat.2025.110065
Hao Zheng , Chunlian Zheng , Chitao Sun , Yudong Zheng , Caiyun Cao , Anqi Zhang , Junpeng Zhang , Hongkai Dang
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引用次数: 0
Integrated analytical framework for soil salinization assessment in the Yellow River Delta coastline: Spatiotemporal dynamics, future trends, and driving mechanisms (2003–2023) 黄河三角洲岸线土壤盐碱化综合分析框架:时空动态、未来趋势及驱动机制(2003-2023)
IF 6.5 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-12-10 DOI: 10.1016/j.agwat.2025.110057
Qizhuo Zhou , Yan Zhou , Danyang Wang , Hongyan Chen , Peng Liu
Coastal salinization threatens arable land where marine influence, shallow groundwater, and cultivation interact. We develop an integrated framework that unifies spatiotemporal trend detection (Sen’s slope–Mann–Kendall), future trend persistence (Hurst exponent), and driver attribution with interactions (GeoDetector) to assess soil salinity content (SSC) in the Yellow River Delta from 2003 to 2023. SSC was mapped annually from Landsat using a random-forest model (validation RMSE 1.55 g kg⁻¹; RPD 1.60). Regional mean SSC declined from 2.46 to 2.20 g kg⁻¹(−10.6 %). Significant improvement covers 46.9 % of land, slight improvement 16.5 %, slight degradation 28.7 %, and significant degradation 3.0 %, indicating predominant improvement with localized relapse. Persistence analysis shows 46.9 % of the area is likely to sustain improvement, 16.5 % has potential to improve, about 29 % is at risk of renewed salinization, and 3 % exhibits persistent degradation; high-risk tracts cluster in southern Guangrao, eastern Wudi, western Zhanhua, and along the Yellow River. Driver attribution ranks the fallow-land ratio as the leading anthropogenic control, and distance to the sea, elevation, evapotranspiration, and silt content as dominant natural drivers; most two-factor combinations show nonlinear enhancement. We conclude that stabilizing cultivation and maintaining drainage underpin durable gains, while risk belts require targeted leaching, drain rehabilitation, and salt-tolerant rotations. By overcoming the separation between change diagnosis, future risk, and governance, this framework couples “where” and “how,” and supports management under different salinization conditions, future trajectories, and dominant drivers in coastal deltas.
在海洋影响、浅层地下水和耕作相互作用的地方,沿海盐碱化威胁着可耕地。我们开发了一个综合框架,将时空趋势检测(Sen’s slope-Mann-Kendall)、未来趋势持续性(Hurst指数)和驱动因素归因与相互作用(GeoDetector)相结合,以评估2003 - 2023年黄河三角洲土壤盐分含量(SSC)。每年从Landsat使用随机森林模型绘制SSC(验证RMSE 1.55 g kg⁻¹;RPD 1.60)。区域平均SSC从2.46下降到2.20 g kg(- 10.6 %)。显著改善46.9% %,轻微改善16.5% %,轻微退化28.7% %,显著退化3.0% %,表现为明显改善,局部复发。持久性分析表明,46.9 %的面积可能持续改善,16.5 %有改善的潜力,约29 %有重新盐渍化的风险,3 %的面积持续退化;高危区集中在广饶南部、武地东部、沾化西部和黄河沿岸。驱动因素归因中,耕地比例是主要的人为控制因素,离海距离、海拔、蒸散量和含沙量是主要的自然驱动因素;大多数双因子组合表现出非线性增强。我们得出结论,稳定种植和保持排水是持久收益的基础,而风险带需要有针对性的淋滤、排水修复和耐盐轮作。通过克服变化诊断、未来风险和治理之间的分离,该框架将“在哪里”和“如何”结合起来,并支持在沿海三角洲不同盐渍化条件、未来轨迹和主要驱动因素下的管理。
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引用次数: 0
Simulation of spatiotemporal variability in nitrate leaching from farmland in the vadose zone of coastal alluvial basin of Dagu River, China 大沽河沿岸冲积盆地渗流带农田硝态氮淋滤时空变化模拟
IF 6.5 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-12-10 DOI: 10.1016/j.agwat.2025.110063
Ke Yang , Hui Peng , Xiao Wang , Meng Jiang
Understanding the spatiotemporal dynamics of groundwater recharge and nitrate leaching driven by agricultural activities is essential for the sustainable management of groundwater resources in agricultural regions. In this study, we developed a regional-scale process-based modeling framework using Hydrus-1D to simulate long-term water flow and nitrate transport in the vadose zone of the Dagu River Basin in eastern coastal China. Groundwater recharge fluxes (21.21–832.31 mm) exhibited strong interannual variability and were significantly correlated with precipitation and irrigation. Nitrate leaching fluxes (9.33–1049.94 kg ha−1 yr−1) closely followed the temporal patterns of groundwater recharge, indicating that recharge is the dominant driver of nitrate leaching dynamics. Spatial variations in groundwater recharge and nitrate leaching were primarily controlled by land-use types and vadose zone thickness. In the vadose zone, water inputs were primarily supplied by precipitation (71.22 %) and irrigation (26.03 %), whereas water outputs were dominated by evapotranspiration (67.77 %) and groundwater recharge (21.40 %). Nitrogen inputs were overwhelmingly derived from chemical fertilizers (94.19 %), with major nitrogen losses occurring through nitrate leaching (29.50 %), root uptake (27.60 %), and denitrification (26.60 %). The deep vadose zone served as an important reservoir for nitrate storage and exerted a significant influence on groundwater quality. These findings provide critical insights for evaluating long-term nitrate contamination risks and developing sustainable nutrient and water management strategies in agricultural landscapes.
了解农业活动驱动下地下水补给和硝态氮淋失的时空动态,对农业地区地下水资源的可持续管理具有重要意义。利用Hydrus-1D建立了基于区域尺度过程的模拟框架,模拟了中国东部沿海大沽河流域水汽带的长期水流和硝酸盐运移。地下水补给通量(21.21 ~ 832.31 mm)表现出较强的年际变化,与降水和灌溉具有显著的相关性。硝酸盐淋滤通量(9.33-1049.94 kg ha−1 yr−1)与地下水补给的时间模式密切相关,表明补给是硝酸盐淋滤动态的主要驱动因素。地下水补给和硝态氮淋滤的空间变化主要受土地利用类型和渗透带厚度的控制。在水汽带,水分输入主要由降水(71.22 %)和灌溉(26.03 %)提供,而水分输出主要由蒸散发(67.77 %)和地下水补给(21.40 %)提供。氮输入绝大多数来自化肥(94.19% %),主要的氮损失发生在硝酸盐淋滤(29.50% %)、根系吸收(27.60% %)和反硝化(26.60% %)。深渗透带是硝酸盐的重要储集层,对地下水水质有重要影响。这些发现为评估长期硝酸盐污染风险和制定可持续的农业景观营养和水管理策略提供了重要见解。
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引用次数: 0
Sustainable exploitation of water resources in the framework of water-energy-food nexus in climate change conditions using new multi-objective optimization algorithm MOGWO-3D 基于MOGWO-3D多目标优化算法的气候变化条件下水-能-粮关系框架下水资源可持续开发
IF 6.5 1区 农林科学 Q1 AGRONOMY Pub Date : 2025-12-10 DOI: 10.1016/j.agwat.2025.110025
Azar Darboei , Arash Azari , Ali Asghar Mirakzadeh
Climate change exerts significant pressure on environmental and socio-economic systems, with water resources being among the most affected. Water, energy, and food form three interdependent pillars within the agricultural sector. Each of these pillars is influenced by climatic variability, and each also contributes to it. Because these components interact in complex ways, their management cannot be separated. So, achieving long-term sustainability requires integrated strategies that consider these interactions. In the Kermanshah Plain, the absence of such an integrated approach has resulted in the unsustainable use of natural resources and growing system instability. System instability denotes the vulnerability of enviroment to disruptions in WEF resourced availability. This research introduces a comprehensive framework for conjunctive surface–groundwater management under climate change conditions using the water-energy-food (WEF) nexus concept. Guided by projections from the Intergovernmental Panel on Climate Change Sixth Assessment Report (IPCC6), the framework simulates future changes in temperature and precipitation. It evaluates the resulting impacts on water availability and develops adaptive strategies for sustainable resource management. A coupled WEAP–MODFLOW model was used to dynamically simulate surface–groundwater interactions across the Kermanshah Plain. Based on these simulations, a multi-objective optimization model was developed using the three-dimensional Multi-Objective Gray Wolf Optimizer (MOGWO-3D). The optimization considered WEF interdependencies and sought the most efficient cropping pattern and resource allocation under projected climate scenarios. System performance was then assessed by comparing the optimized configuration with a reference SSP8.5Hy scenario. The WEF index analysis identified tomatoes, sugar beets, and potatoes as the most influential crops, with correlation coefficients of 0.70, 0.58, and 0.55, respectively. Implementation of the Optimized SSP8.5 Hybrid (Optimized SSP8.5Hy) scenario improved the reliability of meeting agricultural and water demands to 78.4–77.7 %, representing an increase of approximately 19–19.8 % compared with the baseline scenario. Moreover, the simulated groundwater decline was reduced by 9.5 m, indicating a 22 % improvement in subsurface resource stability. Overall, the optimization scenario demonstrated superior performance in maintaining reservoir storage levels, stabilizing groundwater, and sustaining water supply reliability across both dry and wet periods. In addition, the approach mitigated environmental risks associated with agricultural activities, including soil degradation, nutrient runoff, and greenhouse gas emissions. These findings confirm that the proposed simulation–optimization framework provides a robust basis for sustainable water management and agricultural resilience under changing climatic conditions.
气候变化对环境和社会经济系统造成巨大压力,水资源是受影响最大的系统之一。水、能源和粮食是农业部门中相互依存的三大支柱。这些支柱中的每一个都受到气候变化的影响,而且每一个都对气候变化有所贡献。因为这些组件以复杂的方式交互,所以它们的管理不能分离。因此,实现长期可持续性需要综合考虑这些相互作用的战略。在克尔曼沙阿平原,由于缺乏这种综合办法,导致自然资源的不可持续使用和系统日益不稳定。系统不稳定性指的是环境在WEF资源可用性中断时的脆弱性。本研究利用水-能量-食物(WEF)关系概念,提出了气候变化条件下地表水-地下水联合管理的综合框架。该框架以政府间气候变化专门委员会第六次评估报告(IPCC6)的预测为指导,模拟了未来温度和降水的变化。它评估由此产生的对水资源供应的影响,并制定可持续资源管理的适应性战略。采用耦合模型对克尔曼沙平原地表-地下水相互作用进行了动态模拟。在此基础上,利用三维多目标灰狼优化器(MOGWO-3D)建立了多目标优化模型。优化考虑了世界经济论坛的相互依存关系,寻求在预测气候情景下最有效的种植模式和资源配置。然后通过将优化后的配置与参考SSP8.5Hy场景进行比较来评估系统性能。WEF指数分析发现,番茄、甜菜和土豆是影响最大的作物,相关系数分别为0.70、0.58和0.55。优化SSP8.5混合(优化SSP8.5 hy)情景的实施将满足农业和水需求的可靠性提高到78.4 - 77.7% %,与基线情景相比提高了约19-19.8 %。此外,模拟地下水下降量减少了9.5 m,表明地下资源稳定性提高了22. %。总体而言,优化方案在维持水库库容水平、稳定地下水和维持干湿期供水可靠性方面表现优异。此外,该方法还减轻了与农业活动有关的环境风险,包括土壤退化、养分流失和温室气体排放。这些发现证实,所提出的模拟优化框架为气候变化条件下的可持续水资源管理和农业恢复能力提供了坚实的基础。
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引用次数: 0
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Agricultural Water Management
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