在受侵蚀影响的异质农田中测定蒸散量的机器人室系统的好处

IF 5.7 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Adrian Dahlmann, Mathias Hoffmann, Gernot Verch, Marten Schmidt, Michael Sommer, Jürgen Augustin, Maren Dubbert
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引用次数: 0

摘要

摘要鉴于持续的全球气候危机和与之相关的极端水文事件的增加,评估生态系统的复原力以及在农业系统中确保可持续管理和粮食安全至关重要。为此,全面了解生态系统水循环收支和时空动态是必不可少的。蒸散发(ET)在将90%的降水返回大气中起着关键作用。本文研究了土壤类型和管理对农业生态系统季节累积ET (ETsum)和作物单位水分利用效率(WUEagro)的影响。为此,在位于德国东北部乌克尔马克地区丘陵和干地冰碛地貌的侵蚀农田中进行了冬季黑麦的地块试验(2020年9月17日至2021年6月30日)。沿着实验地块(110 m × 16 m),两个封闭的室安装在机器人龙门起重机系统(FluxCrane作为AgroFlux平台的一部分)上,用于确定ET。三种土壤类型代表与丘状地面冰碛景观相关的完整土壤侵蚀梯度(严重侵蚀:Calcaric Regosol;强烈侵蚀:Nudiargic Luvisol;研究了非侵蚀:钙Luvisol)和额外的表土稀释(表土去除和底土外加剂)(随机区组设计,每个处理3个重复)。使用了五种不同的建模方法,并根据它们在整个作物种植期间可靠的ETsum的潜力和再现短期(如昼夜)水通量动态的潜力进行了比较。而机器学习方法,如支持向量机(svm)和人工神经网络(与贝叶斯正则化;ANN_BR)在校准期间通常表现良好,支持向量机在验证期间也提供了令人满意的预测测量ET (k-fold交叉验证,k=5)。我们发现不同土壤类型的干生物量(DM)差异显著,ETsum趋势较小,导致不同的WUEagro。与未被侵蚀的钙质露露醇相比,极度侵蚀的钙质露露醇的ETsum降低了46%,wuegro降低了54%。4月茎秆开始伸长至6月收获,是占总产量70%的关键时期。然而,土壤类型和表土稀释度之间的ETsum差异主要是由于整个栽培过程中处理之间的微小差异造成的,而不仅仅是在这短时间内。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Benefits of a robotic chamber system for determining evapotranspiration in an erosion-affected, heterogeneous cropland
Abstract. In the light of the ongoing global climate crisis and the related increases in extreme hydrological events, it is crucial to assess ecosystem resilience and – in agricultural systems – to ensure sustainable management and food security. For this purpose, a comprehensive understanding of ecosystem water cycle budgets and spatiotemporal dynamics is indispensable. Evapotranspiration (ET) plays a pivotal role in returning up to 90 % of incoming precipitation back to the atmosphere. Here, we studied the impacts of soil types and management on an agroecosystem's seasonal cumulative ET (ETsum) and agronomic water use efficiency (WUEagro, the dry matter per unit of water used by the crop). To do so, a plot experiment with winter rye (17 September 2020 to 30 June 2021) was conducted in an eroded cropland which is located in the hilly and dry ground moraine landscape of the Uckermark region in northeastern Germany. Along the experimental plot (110 m × 16 m), two closed chambers were mounted on a robotic gantry crane system (FluxCrane as part of the AgroFlux platform) and used to determine ET. Three soil types representing the full soil erosion gradient related to the hummocky ground moraine landscape (extremely eroded: Calcaric Regosol; strongly eroded: Nudiargic Luvisol; non-eroded: Calcic Luvisol) and additional topsoil dilution (topsoil removal and subsoil admixture) were investigated (randomized block design, three replicates per treatment). Five different modeling approaches were used and compared in the light of their potential for reliable ETsum over the entire crop cultivation period and to reproduce short-term (e.g., diurnal) water flux dynamics. While machine-learning approaches such as support vector machines (SVMs) and artificial neural networks (with Bayesian regularization; ANN_BR) generally performed well during calibration, SVMs also provided a satisfactory prediction of measured ET during validation (k-fold cross-validation, k=5). We found significant differences in dry biomass (DM) and small trends in ETsum between soil types, resulting in different WUEagro. The extremely eroded Calcaric Regosol showed an up to 46 % lower ETsum and up to 54 % lower WUEagro compared to the non-eroded Calcic Luvisol. The key period contributing to 70 % of ETsum spanned the beginning of stem elongation in April to the harvest in June. However, differences in the ETsum between soil types and topsoil dilution resulted predominantly from small differences between the treatments throughout the cultivation rather than only during this short period of time.
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来源期刊
Hydrology and Earth System Sciences
Hydrology and Earth System Sciences 地学-地球科学综合
CiteScore
10.10
自引率
7.90%
发文量
273
审稿时长
15 months
期刊介绍: Hydrology and Earth System Sciences (HESS) is a not-for-profit international two-stage open-access journal for the publication of original research in hydrology. HESS encourages and supports fundamental and applied research that advances the understanding of hydrological systems, their role in providing water for ecosystems and society, and the role of the water cycle in the functioning of the Earth system. A multi-disciplinary approach is encouraged that broadens the hydrological perspective and the advancement of hydrological science through integration with other cognate sciences and cross-fertilization across disciplinary boundaries.
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