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[江汉平原灌排单元内自然沟渠氮磷浓度动态特征]

[Characteristics of Nitrogen and Phosphorus Concentration Dynamics in Natural Ditches Under an Irrigation-Drainage Unit in the Jianghan Plain].

作者信息

Hua Ling-Ling, Zhang Fu-Lin, Zhai Li-Mei, Liu Hong-Bin, Fan Xian-Peng, Wang Hong-Yuan

机构信息

Key Laboratory of Nonpoint Source Pollution Control, Ministry of Agriculture, Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing 100081, China.

Institute of Plant Protection, Soil and Fertilizer Sciences, Hubei Academy of Agricultural Sciences, Wuhan 430064, China.

出版信息

Huan Jing Ke Xue. 2018 Jun 8;39(6):2715-2723. doi: 10.13227/j.hjkx.201709157.

Abstract

The paddy field in Jianghan Plain usually exists in the form of an irrigation-drainage unit, and the natural ditch is the main part of the unit. A continuous in situ monitoring of the natural ditch water level and water quality through the entire rice growing season in 2015 was conducted to investigate the dynamics of ditch water level and nitrogen and phosphorus concentration in the ditch. Another objective was to determine the effect of these factors. Results showed that during the entire rice growing season, the ditch water depth was maintained between 30 to 70 cm, and the water depth was higher during irrigation events than during rainfall events. Fertilization was the main factor affecting the nitrogen concentration in the ditch water. Two peaks of total nitrogen (TN) concentration appeared on June 18 and July 30 because of topdressing. In the early stage of rice growing, ammonia nitrogen (NH-N) concentration was higher than that of nitrate nitrogen (NO-N). External disturbances (such as rainfall and irrigation events) were the main factors affecting the total phosphorus (TP) concentration in the ditch water. The dynamic of TP concentration in the ditch water was large, and it was consistent with that of the particulate phosphorus (PP) concentration. Drainage of the irrigation-drainage was mainly controlled artificially. The period from rice transplanting to 3 days after the first top dressing was critical in preventing the outflow of ditch water. During the rice harvest stage, the TN and TP concentration were 0.22 and 0.06 mg·L, and the water quality reached theⅡclass standard for surface water quality. This reduced the risk from drainage from the irrigation-drainage unit to the surrounding water environment.

摘要

江汉平原的稻田通常以灌排单元的形式存在,天然沟渠是该单元的主要组成部分。2015年在整个水稻生长季节对天然沟渠水位和水质进行了连续原位监测,以研究沟渠水位动态以及沟渠中氮磷浓度变化。另一个目的是确定这些因素的影响。结果表明,在整个水稻生长季节,沟渠水深保持在30至70厘米之间,灌溉期间的水深高于降雨期间。施肥是影响沟渠水中氮浓度的主要因素。由于追肥,6月18日和7月30日出现了两个总氮(TN)浓度峰值。在水稻生长初期,氨氮(NH-N)浓度高于硝态氮(NO-N)。外部干扰(如降雨和灌溉事件)是影响沟渠水中总磷(TP)浓度的主要因素。沟渠水中TP浓度变化较大,且与颗粒态磷(PP)浓度变化一致。灌排主要通过人工控制。从水稻移栽到第一次追肥后3天这段时间对于防止沟渠水外流至关重要。在水稻收获期,TN和TP浓度分别为0.22和0.06毫克·升,水质达到地表水Ⅱ类标准。这降低了灌排单元排水对周边水环境造成污染的风险。

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