Exogenous phosphorus inputs alter complexity of soil-dissolved organic carbon in agricultural riparian wetlands
Exogenous phosphorus inputs alter complexity of soil-dissolved organic carbon in agricultural riparian wetlands
复制标题
外源磷输入改变农业河岸湿地土壤溶解有机碳的复杂性
DOI:
10.1016/j.chemosphere.2013.09.117
复制
发表时间:
2014
期刊:
影响因子:
8.8
通讯作者:
Schoer Jonathan
中科院分区:
文献类型:
--
作者:
Liu Meng;Zhang Zhijian;He Qiang;Wang Hang;Li Xia;Schoer Jonathan
High-strengthened farmland fertilization leads to mass inputs of nutrients and elements to agricultural riparian wetlands. The dissolved organic carbon (DOC) of such wetland sediments is an important intermediate in global carbon (C) cycling due to its role in connecting soil C pools with atmospheric CO2. But the impact of phosphorus (P) on sediment DOC is still largely unknown, despite increasing investigations to emphasize P interception by riparian wetlands. Here, we simulated the temporal influences of exogenous P on sediment DOC of riparian wetlands by integrating gradient P loading at rates of 0%, 5%, 10%, 20%, 30%, and 60% relative to the initial total phosphorus content of the sediment with the purpose of illustrating the role of external P on the complexity of soil DOC in terms of its amount and composition. After incubating for nine months, a dramatic linear correlation between Olsen-P and fluorescent and ultraviolet spectral indices considered DOC skeleton was observed. Together with a more microbial-derived origin of DOC and a reduction of DOC aromaticity or humicity, the excitation-emission matrix had shown a blue shift reflecting a trend towards a simpler molecular structure of sediment DOC after P addition. Meanwhile, the content of soil DOC and its ratio with total organic carbon (TOC) were also increased by P loading, coupled with enhanced values of highly labile organic carbon and two C-related enzymes. While TOC and recalcitrant organic carbon decreased significantly. Such implications of DOC amounts and composition stimulated by external P loading may enhance its bioavailability, thereby inducing an accelerated effect on soil C cycling and a potential C loss in response to global climate change.