Denitrification potential and its relation to organic carbon quality in three coastal wetland soils

2008 ◽  
Vol 407 (1) ◽  
pp. 471-480 ◽  
Author(s):  
S DODLA ◽  
J WANG ◽  
R DELAUNE ◽  
R COOK
Wetlands ◽  
2016 ◽  
Vol 37 (1) ◽  
pp. 163-175
Author(s):  
Lei Cao ◽  
Jinming Song ◽  
Qidong Wang ◽  
Xuegang Li ◽  
Huamao Yuan ◽  
...  

1996 ◽  
Vol 30 (11) ◽  
pp. 2798-2804 ◽  
Author(s):  
Edelgard W. Pavel ◽  
Raymond B. Reneau ◽  
Duane F. Berry ◽  
Eric P. Smith ◽  
Saied Mostaghimi

2009 ◽  
Vol 41 (3) ◽  
pp. 458-466 ◽  
Author(s):  
Cinzia Fissore ◽  
Christian P. Giardina ◽  
Randall K. Kolka ◽  
Carl C. Trettin

2021 ◽  
Vol 13 (20) ◽  
pp. 4106
Author(s):  
Shuai Wang ◽  
Mingyi Zhou ◽  
Qianlai Zhuang ◽  
Liping Guo

Wetland ecosystems contain large amounts of soil organic carbon. Their natural environment is often both at the junction of land and water with good conditions for carbon sequestration. Therefore, the study of accurate prediction of soil organic carbon (SOC) density in coastal wetland ecosystems of flat terrain areas is the key to understanding their carbon cycling. This study used remote sensing data to study SOC density potentials of coastal wetland ecosystems in Northeast China. Eleven environmental variables including normalized difference vegetation index (NDVI), difference vegetation index (DVI), soil adjusted vegetation index (SAVI), renormalization difference vegetation index (RDVI), ratio vegetation index (RVI), topographic wetness index (TWI), elevation, slope aspect (SA), slope gradient (SG), mean annual temperature (MAT), and mean annual precipitation (MAP) were selected to predict SOC density. A total of 193 soil samples (0–30 cm) were divided into two parts, 70% of the sampling sites data were used to construct the boosted regression tree (BRT) model containing three different combinations of environmental variables, and the remaining 30% were used to test the predictive performance of the model. The results show that the full variable model is better than the other two models. Adding remote sensing-related variables significantly improved the model prediction. This study revealed that SAVI, NDVI and DVI were the main environmental factors affecting the spatial variation of topsoil SOC density of coastal wetlands in flat terrain areas. The mean (±SD) SOC density of full variable models was 18.78 (±1.95) kg m−2, which gradually decreased from northeast to southwest. We suggest that remote sensing-related environmental variables should be selected as the main environmental variables when predicting topsoil SOC density of coastal wetland ecosystems in flat terrain areas. Accurate prediction of topsoil SOC density distribution will help to formulate soil management policies and enhance soil carbon sequestration.


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