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[潮汐对中国东南部闽江河口土壤及孔隙水中硅和氮含量的影响]

[Influences of tide on silicon and nitrogen contents in soil and porewater in the Minjiang Ri-ver estuary, Southeast China].

作者信息

Hou Guan Yun, Zhai Shui Jing, Le Xiao Qing, Tong Chuan

机构信息

School of Geographical Science, Fujian Normal University, Fuzhou 350007, China.

Research Center of Wetlands in Subtropical Region, Fujian Normal University, Fuzhou 350007, China.

出版信息

Ying Yong Sheng Tai Xue Bao. 2017 Jan;28(1):337-344. doi: 10.13287/j.1001-9332.201701.002.

DOI:10.13287/j.1001-9332.201701.002
PMID:29749219
Abstract

Taking Shanyuntan wetland in the Minjiang River estuary as test object, the dissolved silicates (DSi) and inorganic nitrogen contents in porewater and the biogenic silica (BSi) and total nitrogen contents in surface soil of the Phragmites australis wetland, Cyperus malaccensis wetland and Spartina alterniflora wetland were measured in October 2014 (spring tide month) and April 2015 (neap tide month), respectively, to illuminate the influence of tide on silicon and nitrogen contents in soil and porewater of estuarine wetland. Results showed that the DSi content in porewater and the BSi content in surface soil in spring tide month were slightly higher than those in neap tide month, with the highest being observed on neap tide day and the lowest occurring on spring tide day. In contrast, the BSi content in surface soil on spring tide day showed an opposite trend with that on neap tide day. The contents of NH-N and NO-N in porewater of different wetland soils in spring tide month were higher than those in neap tide month, while the content of NH-N on spring tide day was significantly higher than that on neap tide day (P<0.05). The study found that hydrological conditions such as flooding duration and drying-wetting alternation caused by tide had great influences on silicon and nitrogen contents in porewater and surface soil, and vegetation types also showed great influences on their distributions in intertidal wetland of the Minjiang River estuary.

摘要

以闽江河口鳝鱼滩湿地为研究对象,分别于2014年10月(大潮月)和2015年4月(小潮月)测定了芦苇湿地、咸水草湿地和互花米草湿地孔隙水中的溶解硅酸盐(DSi)和无机氮含量,以及表层土壤中的生物源二氧化硅(BSi)和总氮含量,以阐明潮汐对河口湿地土壤和孔隙水中硅和氮含量的影响。结果表明,大潮月孔隙水中的DSi含量和表层土壤中的BSi含量略高于小潮月,最高值出现在小潮日,最低值出现在大潮日。相反,大潮日表层土壤中的BSi含量与小潮日呈相反趋势。大潮月不同湿地土壤孔隙水中的NH-N和NO-N含量高于小潮月,而大潮日的NH-N含量显著高于小潮日(P<0.05)。研究发现,潮汐引起的淹没持续时间和干湿交替等水文条件对孔隙水和表层土壤中的硅和氮含量有很大影响,植被类型对闽江河口潮间带湿地中它们的分布也有很大影响。

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