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季节性冻结农业流域解冻期氮素输出规律。

Patterns of nitrogen export from a seasonal freezing agricultural watershed during the thawing period.

机构信息

State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, 430072 Wuhan, Hubei, China.

State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, 430072 Wuhan, Hubei, China.

出版信息

Sci Total Environ. 2017 Dec 1;599-600:442-450. doi: 10.1016/j.scitotenv.2017.04.174. Epub 2017 May 5.

Abstract

The objectives of this study were to investigate water, ammonium nitrogen (NH-N), and nitrate nitrogen (NO-N) export processes during the thawing period in a watershed with heavy agricultural activities and to evaluate contributions of N (i.e., NO-N and NH-N) from different source areas under different climate conditions. Experiments were conducted within the 75km agricultural Heidingzi watershed in northeast China. The thawing period was divided into four stages: early-melt, late-melt, rain-on-melt, and post-melt. Drainage regions (DRs) were separated into three types. The processes of water and N discharge from soil into rivers were monitored in these DRs during the thawing periods of 2014, 2015, and 2016. Results show that the processes of water and N discharge were not synchronous during the thawing period. Variations in discharge concentrations of NH-N and NO-N during the thawing period were mainly affected by the flushing effect, which was controlled by the physical state of the surface water (snow or ice) and the melt rate of frozen soil. Contributions of N export from the DRs varied under different land uses and climate conditions during the thawing period. NO-N export was mainly from maize fields. Thawing stages with high NO-N export were always accompanied by higher discharge rates. NH-N export mainly occurred during the early-melt and late-melt stages and from riverside rural regions.

摘要

本研究的目的是在一个农业活动频繁的流域,研究融雪期的水、氨氮(NH-N)和硝酸盐氮(NO-N)的输出过程,并评估不同气候条件下不同源区氮(即 NO-N 和 NH-N)的贡献。实验在中国东北的 75 公里长的农业黑顶子流域进行。融雪期分为四个阶段:早期融化、晚期融化、雨融化和融化后。排水区(DR)分为三种类型。在 2014、2015 和 2016 年的融雪期,监测了这些 DR 中土壤向河流排放水和 N 的过程。结果表明,融雪期的水和 N 排放过程不同步。融雪期 NH-N 和 NO-N 排放浓度的变化主要受冲洗效应的影响,冲洗效应受地表水(雪或冰)的物理状态和冻土融化率控制。在融雪期,不同土地利用和气候条件下,DR 中 N 输出的贡献不同。NO-N 主要来自玉米地。NO-N 输出较高的融雪阶段通常伴随着更高的排放速率。NH-N 主要在早期融化和晚期融化阶段以及河边农村地区排放。

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