Sun Zhi Gao, Sun Wen Guang
Institute of Geo-graphy/Ministry of Education Key Laboratory of Humid Subtropical Eco-geographical Process, Fujian Normal University, Fuzhou 350007, China.
School of Plant, Environment and Soil Science, Louisiana State University, Baton Rouge 70803, USA.
Ying Yong Sheng Tai Xue Bao. 2016 Apr 22;27(4):1135-1144. doi: 10.13287/j.1001-9332.201604.030.
The effects of exogenous nitrogen on NO production processes in the soils of un-restoration wetland (R), restoration wetland since 2007 (R) and restoration wetland since 2002 (R) of the Yellow River estuary were studied, and the contributions of different processes in NO production were determined. Results showed that the NO production of restoration wetland soils (R and R) with NO-N addition was much higher than that with NH-N addition, but both NH-N and NO-N additions demonstrated inhibition on the NO production of soils in R. Although the effect of NO-N addition on the total NO production of topsoil in R was significantly higher than those in R, the values in R and R were greatly increased with increasing NO-N addition. The denitrification and nitrifier denitrification processes in restoration wetland soils (R and R) were greatly affected by NO-N addition, but no significant influence on the non-biological processes of soil in R was observed. Although NH-N addition did not produce significant effects on the total NO production of wetland soils, the nitrifier denitrification process in R soil, the nitrification process in R soil and the non-biological process in R soil were generally stimulated. In R and R soils, the NO produced by non-biological processes was generally eleva-ted with NH-N addition, while with NO-N addition, the non-biological processes generating NO in R, R and R soils were generally inhibited, which was closely correlated with the regulation of soil pH caused by the import of exogenous nitrogen. This study found that the enrichment of NO-N greatly enhanced the total NO production of wetland soils and significantly altered the original contribution patterns of biological and non-biological processes to NO production. Thus, special attention should be paid on the influences of nutrient import (particularly NO-N enrichment) induced by ecological restoration project on NO production of wetland soils.
研究了外源氮对黄河口未恢复湿地(R)、2007年以来的恢复湿地(R)和2002年以来的恢复湿地(R)土壤中NO产生过程的影响,并确定了不同过程对NO产生的贡献。结果表明,添加NO-N的恢复湿地土壤(R和R)的NO产生量远高于添加NH-N的情况,但添加NH-N和NO-N均对R中土壤的NO产生有抑制作用。虽然添加NO-N对R表土总NO产生的影响显著高于R,但R和R中的值随着NO-N添加量的增加而大幅增加。添加NO-N对恢复湿地土壤(R和R)中的反硝化和硝化细菌反硝化过程影响很大,但未观察到对R中土壤非生物过程的显著影响。虽然添加NH-N对湿地土壤总NO产生没有显著影响,但R土壤中的硝化细菌反硝化过程、R土壤中的硝化过程和R土壤中的非生物过程总体上受到刺激。在R和R土壤中,添加NH-N通常会使非生物过程产生的NO升高,而添加NO-N时,R、R和R土壤中产生NO的非生物过程通常受到抑制,这与外源氮输入引起的土壤pH调节密切相关。本研究发现,NO-N的富集极大地提高了湿地土壤的总NO产生量,并显著改变了生物和非生物过程对NO产生的原始贡献模式。因此,应特别关注生态恢复工程引起的养分输入(特别是NO-N富集)对湿地土壤NO产生的影响。