Soil Processes and Current Trends in Quality Assessment 2013
DOI: 10.5772/53211
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Estimation of Soil Carbon Stock in Taiwan Arable Soils by Using Legacy Database and Digital Soil Mapping

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Cited by 6 publications
(6 citation statements)
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“…Crop rotation, tillage, and fertilization change the inputs and outputs and, consequently, the entire dynamics of SOM in agricultural soils [8][9][10]. These changes release considerable amounts of carbon dioxide (CO 2 ), nitrous oxide (N 2 O), and methane (CH 4 ) into the atmosphere, contributing to a global mean production intensity of 0.16 Mg CO 2 e M kcal −1 [11], with a negative impact on global climate.…”
Section: Introductionmentioning
confidence: 99%
“…Crop rotation, tillage, and fertilization change the inputs and outputs and, consequently, the entire dynamics of SOM in agricultural soils [8][9][10]. These changes release considerable amounts of carbon dioxide (CO 2 ), nitrous oxide (N 2 O), and methane (CH 4 ) into the atmosphere, contributing to a global mean production intensity of 0.16 Mg CO 2 e M kcal −1 [11], with a negative impact on global climate.…”
Section: Introductionmentioning
confidence: 99%
“…Tsai et al ( 2010 ) and Jien et al ( 2010 ) estimated SOC stocks of 63 forest soils (excluding Histosols and Spodosols) and 140 cropland soils in the upper 100 cm depth, indicating that converting forestlands to croplands can significantly result in SOC stocks loss. Tsui et al ( 2013 ) also estimated the SOC stocks under bamboo, grass, and secondary forests with the different elevation between 300 and 1000 m for Andisols and Inceptisols in Yangingshan National Park in northern Taiwan and suggested that elevation is a simple and effective predictor of SOC stocks. Lin et al ( 2016 ) investigated SOC stocks in afforested and abandoned fields at different elevation and found that SOC stocks varied with elevation, land use, and soil depth.…”
Section: Introductionmentioning
confidence: 99%
“…They are important for determining the PBDE’s affinity to solids, as a higher organic carbon content gives soils and sediments a higher capacity for PBDE partitioning due to the absorbent nature of carbon. The fraction organic carbon (F oc ) content for soil was obtained using an average value of soil organic carbon measurements taken in the Changhua region of Taiwan which was calculated to be 0.0121 (Tsui et al 2013 ). The F oc for sediment was calculated to be 0.00752 from the conversion of the average of 30 values taken along the southwest coast of Taiwan (Kao et al 2006 ).…”
Section: Methodsmentioning
confidence: 99%