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中国东部沿海大规模围填海后不同类型围填海区土壤有机碳氮库演变。

Shift in soil organic carbon and nitrogen pools in different reclaimed lands following intensive coastal reclamation on the coasts of eastern China.

机构信息

College of Life Sciences, Shaanxi Normal University, Xi'an, 710119, P. R. China.

School of Life Science and Institute of Wetland Ecology, Nanjing University, Nanjing, 210023, P. R. China.

出版信息

Sci Rep. 2019 Apr 11;9(1):5921. doi: 10.1038/s41598-019-42048-6.

Abstract

The impacts of coastal reclamation on carbon (C) and nitrogen (N) sinks of coastal wetlands remain unclearly understood. This study was conducted to investigate the alterations of soil organic C and N (SOC and SON) pools following conversion of Phragmites australis salt marsh into fishpond, wheat and rapeseed fields and town construction land through reclamation along Jiangsu coast in eastern China. Coastal reclamation significantly increased stocks of soil total, labile and recalcitrant organic C and N (SLOC, SLON, SROC, and SRON), and concentrations of water-soluble organic C (WSOC), microbial biomass C and N (SMBC and SMBN), cumulative CO-C mineralization (MINC) following conversion of P. australis salt marsh into fishpond, wheat and rapeseed fields. However, coastal reclamation reduced SOC, SLOC, SROC, SRON, WSOC, SMBC, SMBN, and MINC following conversion of P. australis salt marsh into town construction land. Our results suggest that coastal reclamation affects C and N sinks of coastal wetlands by changing SOC and SON pools size, stability and dynamics changes following conversion of P. australis salt marsh into other land use types. This finding were primarily attributed to alterations in quantity and quality of exogenous materials returning the soil, and soil physiochemical properties as affected by coastal reclamation.

摘要

填海造地对滨海湿地碳(C)和氮(N)汇的影响尚不清楚。本研究旨在调查江苏沿海填海造地将芦苇盐沼转化为鱼塘、小麦和油菜田以及城镇建设用地后土壤有机碳和氮(SOC 和 SON)库的变化。填海造地显著增加了土壤总、易变和难降解有机碳和氮(SLOC、SLON、SROC 和 SRON)以及水溶性有机碳(WSOC)、微生物生物量 C 和 N(SMBC 和 SMBN)、累积 CO-C 矿化(MINC)的储量,随后将芦苇盐沼转化为鱼塘、小麦和油菜田。然而,填海造地将芦苇盐沼转化为城镇建设用地后,SOC、SLOC、SROC、SRON、WSOC、SMBC、SMBN 和 MINC 减少。我们的研究结果表明,填海造地通过改变 SOC 和 SON 库的大小、稳定性和芦苇盐沼转化为其他土地利用类型后的动态变化,影响滨海湿地的碳和氮汇。这一发现主要归因于返回土壤的外源物质的数量和质量以及填海造地对土壤理化性质的改变。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8c9e/6459922/e45441c582d8/41598_2019_42048_Fig1_HTML.jpg

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