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中国东部农业排水河中氮磷的季节性滞留。

Seasonal variations of nitrogen and phosphorus retention in an agricultural drainage river in East China.

机构信息

Department of Natural Resources, College of Environmental Science and Natural Resources, Zhejiang University, KaiXuan Road 258#, Hangzhou, 310029, Zhejiang Province, People's Republic of China.

出版信息

Environ Sci Pollut Res Int. 2010 Feb;17(2):312-20. doi: 10.1007/s11356-009-0246-x. Epub 2009 Oct 1.

Abstract

BACKGROUND, AIM, AND SCOPE: Riverine retention decreases loads of nitrogen (N) and phosphorus (P) in running water. It is an important process in nutrient cycling in watersheds. However, temporal riverine nutrient retention capacity varies due to changes in hydrological, ecological, and nutrient inputs into the watershed. Quantitative information of seasonal riverine N and P retention is critical for developing strategies to combat diffuse source pollution and eutrophication in riverine and coastal systems. This study examined seasonal variation of riverine total N (TN) and total P (TP) retention in the ChangLe River, an agricultural drainage river in east China.

METHODS

Water quality, hydrological parameters, and hydrophyte coverage were monitored along the ChangLe River monthly during 2004-2006. Nutrient export loads (including chemical fertilizer, livestock, and domestic sources) entering the river from the catchment area were computed using an export coefficient model based on estimated nutrient sources. Riverine TN and TP retention loads (RNRL and RPRL) were estimated using mass balance calculations. Temporal variations in riverine nutrient retention were analyzed statistically.

RESULTS AND DISCUSSION

Estimated annual riverine retention loads ranged from 1,538 to 2,127 t year(-1) for RNRL and from 79.4 to 90.4 t year(-1) for RPRL. Monthly retention loads varied from 6.4 to 300.8 t month(-1) for RNRL and from 1.4 to 15.3 t month(-1) for RPRL. Both RNRL and RPRL increased with river flow, water temperature, hydrophyte coverage, monthly sunshine hours, and total TN and TP inputs. Dissolved oxygen concentration and the pH level of the river water decreased with RNRL and RPRL. Riverine nutrient retention ratios (retention as a percentage of total input) were only related to hydrophyte coverage and monthly sunshine hours. Monthly variations in RNRL and RPRL were functions of TN and TP loads.

CONCLUSIONS

Riverine nutrient retention capacity varied with environmental conditions. Annual RNRL and RPRL accounted for 30.3-48.3% and 52.5-71.2%, respectively, of total input TN and TP loads in the ChangLe River. Monthly riverine retention ratios were 3.5-88.7% for TN and 20.5-92.6% for TP. Hydrophyte growth and coverage on the river bed is the main cause for seasonal variation in riverine nutrient retention capacity. The total input TN and TP loads were the best indicators of RNRL and RPRL, respectively.

RECOMMENDATIONS AND PERSPECTIVES

High riverine nutrient retention capacity during summer due to hydrophytic growth is favorable to the avoidance of algal bloom in both river systems and coastal water in southeast China. Policies should be developed to strictly control nutrient applications on agricultural lands. Strategies for promoting hydrophyte growth in rivers are desirable for water quality management.

摘要

背景、目的和范围:河流滞留减少了流水体中的氮(N)和磷(P)负荷。它是流域养分循环中的一个重要过程。然而,由于水文、生态和养分输入到流域的变化,河流养分滞留能力随时间而变化。定量了解季节性河流 N 和 P 滞留对于制定策略以对抗河流和沿海系统中面源污染和富营养化至关重要。本研究调查了中国东部农业排水河流昌乐河的季节性河流总氮(TN)和总磷(TP)滞留变化。

方法

2004 年至 2006 年期间,每月沿昌乐河监测水质、水文参数和水生植物覆盖率。根据估计的养分来源,使用基于出口系数模型计算从流域进入河流的养分出口负荷(包括化肥、牲畜和家庭来源)。利用质量平衡计算估计河流 TN 和 TP 滞留负荷(RNRL 和 RPRL)。使用统计方法分析河流养分滞留的时间变化。

结果与讨论

估计的年河流滞留负荷范围为 1538 至 2127 t 年(-1)用于 RNRL 和 79.4 至 90.4 t 年(-1)用于 RPRL。每月的滞留负荷范围为 6.4 至 300.8 t 月(-1)用于 RNRL 和 1.4 至 15.3 t 月(-1)用于 RPRL。RNRL 和 RPRL 均随河流流量、水温和水生植物覆盖率、每月日照小时数以及总 TN 和 TP 输入而增加。河流水中的溶解氧浓度和 pH 值随 RNRL 和 RPRL 而降低。河流养分滞留率(作为总输入的百分比的滞留)仅与水生植物覆盖率和每月日照小时数有关。RNRL 和 RPRL 的月变化是 TN 和 TP 负荷的函数。

结论

河流养分滞留能力随环境条件而变化。昌乐河的年 RNRL 和 RPRL 分别占 TN 和 TP 总输入负荷的 30.3-48.3%和 52.5-71.2%。每月的河流滞留率分别为 TN 的 3.5-88.7%和 TP 的 20.5-92.6%。河床水生植物的生长和覆盖是河流养分滞留能力季节性变化的主要原因。总输入 TN 和 TP 负荷分别是 RNRL 和 RPRL 的最佳指标。

建议和展望

夏季由于水生植物的生长而导致的高河流养分滞留能力有利于避免中国东南部河流和沿海水域的藻类大量繁殖。应制定政策严格控制农业用地的养分施用。促进河流中水生植物生长的策略是水质管理的理想选择。

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