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集约化灌溉农业下流域尺度氮负荷减少的机制

Mechanisms of basin-scale nitrogen load reductions under intensified irrigated agriculture.

作者信息

Törnqvist Rebecka, Jarsjö Jerker, Thorslund Josefin, Rao P Suresh C, Basu Nandita B, Destouni Georgia

机构信息

Department of Physical Geography and Quaternary Geology and the Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden.

School of Civil Engineering and Department of Agronomy, Purdue University, West Lafayette, West Lafayette, Indiana, United States of America.

出版信息

PLoS One. 2015 Mar 19;10(3):e0120015. doi: 10.1371/journal.pone.0120015. eCollection 2015.

Abstract

Irrigated agriculture can modify the cycling and transport of nitrogen (N), due to associated water diversions, water losses, and changes in transport flow-paths. We investigate dominant processes behind observed long-term changes in dissolved inorganic nitrogen (DIN) concentrations and loads of the extensive (465,000 km2) semi-arid Amu Darya River basin (ADRB) in Central Asia. We specifically considered a 40-year period (1960-2000) of large irrigation expansion, reduced river water flows, increased fertilizer application and net increase of N input into the soil-water system. Results showed that observed decreases in riverine DIN concentration near the Aral Sea outlet of ADRB primarily were due to increased recirculation of irrigation water, which extends the flow-path lengths and enhances N attenuation. The observed DIN concentrations matched a developed analytical relation between concentration attenuation and recirculation ratio, showing that a fourfold increase in basin-scale recirculation can increase DIN attenuation from 85 to 99%. Such effects have previously only been observed at small scales, in laboratory experiments and at individual agricultural plots. These results imply that increased recirculation can have contributed to observed increases in N attenuation in agriculturally dominated drainage basins in different parts of the world. Additionally, it can be important for basin scale attenuation of other pollutants, including phosphorous, metals and organic matter. A six-fold lower DIN export from ADRB during the period 1981-2000, compared to the period 1960-1980, was due to the combined result of drastic river flow reduction of almost 70%, and decreased DIN concentrations at the basin outlet. Several arid and semi-arid regions around the world are projected to undergo similar reductions in discharge as the ADRB due to climate change and agricultural intensification, and may therefore undergo comparable shifts in DIN export as shown here for the ADRB. For example, projected future increases of irrigation water withdrawals between 2005 and 2050 may decrease the DIN export from arid world regions by 40%.

摘要

由于相关的水资源调配、水流失以及水流路径的变化,灌溉农业会改变氮(N)的循环和迁移。我们研究了中亚广袤(46.5万平方公里)的半干旱阿姆河盆地(ADRB)中观测到的溶解无机氮(DIN)浓度和负荷长期变化背后的主导过程。我们特别考虑了一个40年的时期(1960 - 2000年),在此期间灌溉大幅扩张、河流水量减少、化肥施用量增加以及土壤 - 水系统中的氮输入净增加。结果表明,ADRB咸海出口附近河流水体中DIN浓度的观测下降主要是由于灌溉水再循环增加,这延长了水流路径长度并增强了氮的衰减。观测到的DIN浓度与浓度衰减和再循环率之间建立的分析关系相匹配,表明流域尺度再循环增加四倍可使DIN衰减从85%增至99%。此前这种效应仅在小规模的实验室实验和个别农田中观测到。这些结果意味着再循环增加可能促成了世界不同地区以农业为主的流域中观测到的氮衰减增加。此外,对于包括磷、金属和有机物在内的其他污染物的流域尺度衰减也可能很重要。与1960 - 1980年期间相比,1981 - 2000年期间ADRB的DIN输出降低了六倍,这是河流水量急剧减少近70%以及流域出口处DIN浓度降低的综合结果。由于气候变化和农业集约化,预计世界上几个干旱和半干旱地区的径流量将经历与ADRB类似的减少,因此DIN输出可能会发生与此处ADRB所示类似的变化。例如,预计2005年至2050年灌溉取水量的未来增加可能使干旱世界地区的DIN输出减少40%。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5dc7/4366109/ec11af7c9765/pone.0120015.g001.jpg

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