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恢复湿地中硝酸盐去除过程的强化。

Stimulating nitrate removal processes of restored wetlands.

机构信息

Department of Environmental Studies, Mount Holyoke College , South Hadley, Massachusetts 01075, United States.

出版信息

Environ Sci Technol. 2014 Jul 1;48(13):7365-73. doi: 10.1021/es500799v. Epub 2014 Jun 10.

DOI:10.1021/es500799v
PMID:24915604
Abstract

The environmental and health effects caused by nitrate contamination of aquatic systems are a serious problem throughout the world. A strategy proposed to address nitrate pollution is the restoration of wetlands. However, although natural wetlands often remove nitrate via high rates of denitrification, wetlands restored for water quality functions often fall below expectations. This may be in part because key drivers for denitrification, in particular soil carbon, are slow to develop in restored wetlands. We added organic soil amendments that range along a gradient of carbon lability to four newly restored wetlands in western New York to investigate the effect of carbon additions on denitrification and other processes of the nitrogen cycle. Soil carbon increased by 12.67-63.30% with the use of soil amendments (p ≤ 0.0001). Soil nitrate, the carbon to nitrogen ratio, and microbial biomass nitrogen were the most significant predictors of denitrification potential. Denitrification potential, potential net nitrogen nitrification and mineralization, and soil nitrate and ammonium, were highest in topsoil-amended plots, with increases in denitrification potential of 161.27% over control plots. While amendment with topsoil more than doubled several key nitrogen cycling processes, more research is required to determine what type and level of amendment application are most effective for stimulating removal of exogenous nitrate and meeting functional goals within an acceptable time frame.

摘要

水生系统中硝酸盐污染造成的环境和健康影响是一个全球性的严重问题。人们提出了一种策略来解决硝酸盐污染问题,即恢复湿地。然而,尽管天然湿地通常通过高硝酸盐去除率来去除硝酸盐,但为水质功能而恢复的湿地往往达不到预期的效果。这可能部分是因为对于反硝化作用而言非常关键的驱动因素(特别是土壤碳)在恢复湿地中发展缓慢。我们向纽约西部的四个新恢复的湿地中添加了一系列从碳惰性到活性逐渐增强的有机土壤改良剂,以研究碳添加对反硝化作用和氮循环其他过程的影响。使用土壤改良剂后土壤碳增加了 12.67-63.30%(p ≤ 0.0001)。土壤硝酸盐、碳氮比和微生物生物量氮是反硝化潜力的最主要预测因子。与对照样地相比,表层土添加样地的反硝化潜力、净氮硝化和矿化潜力以及土壤硝酸盐和铵盐最高,反硝化潜力增加了 161.27%。虽然表层土添加改良剂使几个关键的氮循环过程增加了一倍以上,但仍需要进一步研究,以确定哪种类型和水平的添加改良剂应用最能有效地刺激外源硝酸盐的去除,并在可接受的时间框架内实现功能目标。

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