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添加氮和硫酸盐对中国东南闽江河口高位沼泽湿地 CH 和 CO 排放、土壤和孔隙水化学的影响。

Effects of the addition of nitrogen and sulfate on CH and CO emissions, soil, and pore water chemistry in a high marsh of the Min River estuary in southeastern China.

机构信息

School of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China; Key Laboratory of Humid Sub-tropical Eco-geographical Process of Ministry of Education, Fujian Normal University, Fuzhou 350007, China; Research Centre of Wetlands in Subtropical Region, Fujian Normal University, Fuzhou 350007, China.

Department of Biological Sciences, Florida International University, Miami, FL 33199, USA.

出版信息

Sci Total Environ. 2017 Feb 1;579:292-304. doi: 10.1016/j.scitotenv.2016.11.103. Epub 2016 Nov 25.

DOI:10.1016/j.scitotenv.2016.11.103
PMID:27894801
Abstract

Exogenous nitrogen (N) and sulfate (SO), resulting from human activity, can strongly influence the emission of CH and CO from soil ecosystems. Studies have reported the effects of N and SO on CH and CO emissions from inland peatlands and paddies. However, very few studies have presented year-round data on the effects of the addition of N and SO on CH and CO emissions in estuarine marshes. The effects of the addition of N and SO on the emission of CH and CO were investigated in a Cyperus malaccensis marsh in the high tidal flat of the Min River estuary of southeastern China from September 2014 to August 2015. Dissolved NHCl, KNO, and KSO were applied every month, in doses of 24gN/SOm·yr. The emission of CH and CO showed distinct monthly and seasonal variations. Compared with the control, the addition of NHCl and NHNO+KSO showed increases in CH fluxes (p<0.05), while the effects of the addition of KNO and KSO on CH were minor (p>0.05). NHCl had a positive impact on CO emissions (p<0.01), while the addition of KNO, KSO, and NHNO+KSO had minor positive impacts, compared to the control (p>0.05). Correlation analysis found that soil sulfate concentration, nitrogen availability and enzyme activity were the dominant factors influencing CH and CO variation. Our findings suggest that CH and CO emissions were influenced more by ammonium than by nitrate. We propose that the suppressive effect of additional sulfate on CH production is insignificant, due to which the inhibition may be overestimated in the estuarine brackish marsh.

摘要

外源氮 (N) 和硫酸盐 (SO) 是人类活动的产物,它们可以强烈影响土壤生态系统中 CH 和 CO 的排放。研究报道了 N 和 SO 对内陆泥炭地和稻田中 CH 和 CO 排放的影响。然而,很少有研究提供关于在河口沼泽中添加 N 和 SO 对 CH 和 CO 排放的全年数据。本研究于 2014 年 9 月至 2015 年 8 月在中国东南闽江河口高滩的一种短叶茳芏沼泽中,调查了添加 N 和 SO 对 CH 和 CO 排放的影响。每月以 24gN/SOm·yr 的剂量添加溶解的 NHCl、KNO 和 KSO。CH 和 CO 的排放表现出明显的月度和季节性变化。与对照相比,添加 NHCl 和 NHNO+KSO 增加了 CH 通量(p<0.05),而添加 KNO 和 KSO 对 CH 的影响较小(p>0.05)。NHCl 对 CO 排放有积极影响(p<0.01),而与对照相比,添加 KNO、KSO 和 NHNO+KSO 则有较小的积极影响(p>0.05)。相关性分析发现,土壤硫酸盐浓度、氮素有效性和酶活性是影响 CH 和 CO 变化的主要因素。我们的研究结果表明,CH 和 CO 的排放受铵盐的影响大于硝酸盐。我们提出,由于额外硫酸盐对 CH 生成的抑制作用不明显,因此在河口盐沼中可能高估了这种抑制作用。

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