Sub-tropic degraded red soil restoration: Is soil organic carbon build-up limited by nutrients supply

2013 ◽  
Vol 300 ◽  
pp. 77-87 ◽  
Author(s):  
Xia Gong ◽  
Yuanqiu Liu ◽  
Qinglin Li ◽  
Xiaohua Wei ◽  
Xiaomin Guo ◽  
...  
Pedosphere ◽  
2011 ◽  
Vol 21 (2) ◽  
pp. 207-213 ◽  
Author(s):  
Dong-Sheng YU ◽  
Zhong-Qi ZHANG ◽  
Hao YANG ◽  
Xue-Zheng SHI ◽  
Man-Zhi TAN ◽  
...  

CATENA ◽  
2020 ◽  
Vol 190 ◽  
pp. 104547
Author(s):  
Yue Zhang ◽  
Dongfeng Zhao ◽  
Jinshi Lin ◽  
Lin Jiang ◽  
Bifei Huang ◽  
...  

2018 ◽  
Vol 10 (10) ◽  
pp. 3603 ◽  
Author(s):  
Zhongqi Zhang ◽  
Yiquan Sun ◽  
Dongsheng Yu ◽  
Peng Mao ◽  
Li Xu

Research on the regional variability of soil organic carbon (SOC) has focused mostly on the influence of the number of soil sampling points and interpolation methods. Little attention has typically been paid to the influence of sampling point discretization. Based on dense soil sampling points in the red soil area of Southern China, we obtained four sample discretization levels by a resampling operation. Then, regional SOC distributions were obtained at four levels by two interpolation methods: ordinary Kriging (OK) and Kriging combined with land use information (LuK). To evaluate the influence of sample discretization on revealing SOC variability, we compared the interpolation accuracies at four discretization levels with uniformly distributed validation points. The results demonstrated that the spatial distribution patterns of SOC were roughly similar, but the contour details in some local areas were different at the various discretization levels. Moreover, the predicted mean absolute errors (MAE) and root mean square errors (RMSE) of the two Kriging methods all rose with an increase in discretization. From the lowest to the largest discretization level, the MAEs of OK and LuK rose from 4.47 and 3.02 g kg−1 to 5.46 and 3.54 g kg−1, and the RMSEs rose from 5.13 and 3.95 g kg−1 to 5.76 and 4.76 g kg−1, respectively. Though the trend of prediction errors varied with discretization levels, the interpolation accuracies of the two Kriging methods were both influenced by the sample discretization level. Furthermore, the spatial interpolation uncertainty of OK was more sensitive to the discretization level than that of the LuK method. Therefore, when the spatial distribution of SOC is predicted using Kriging methods based on the same sample quantity, the more uniformly distributed sampling points are, the more accurate the spatial prediction accuracy of SOC will be, and vice versa. The results of this study can act as a useful reference for evaluating the uncertainty of SOC spatial interpolation and making a soil sampling scheme in the red soil region of China.


2017 ◽  
Vol 37 (1) ◽  
Author(s):  
朱丽琴 ZHU Liqin ◽  
黄荣珍 HUANG Rongzhen ◽  
段洪浪 DUAN Honglang ◽  
贾龙 JIA Long ◽  
王赫 WANG He ◽  
...  

2020 ◽  
Vol 72 (1) ◽  
pp. 446-459 ◽  
Author(s):  
Jinyue Bai ◽  
Mingming Zong ◽  
Shiyu Li ◽  
Haixia Li ◽  
Changqun Duan ◽  
...  

Geomorphology ◽  
2013 ◽  
Vol 197 ◽  
pp. 137-144 ◽  
Author(s):  
Xue Zhang ◽  
Zhongwu Li ◽  
Zhenghong Tang ◽  
Guangming Zeng ◽  
Jinquan Huang ◽  
...  

2013 ◽  
Vol 33 (10) ◽  
pp. 2964-2973 ◽  
Author(s):  
何圣嘉 HE Shengjia ◽  
谢锦升 XIE Jinsheng ◽  
曾宏达 ZENG Hongda ◽  
田浩 TIAN Hao ◽  
周艳翔 ZHOU Yanxiang ◽  
...  

2018 ◽  
Vol 10 (7) ◽  
pp. 2290 ◽  
Author(s):  
Zhongqi Zhang ◽  
Dongsheng Yu ◽  
Xiyang Wang ◽  
Yue Pan ◽  
Guangxing Zhang ◽  
...  

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