Predicting Soil Organic Carbon Stock Using Profile Depth Distribution Functions and Ordinary Kriging

被引:160
作者
Mishra, Umakant [1 ]
Lal, Rattan [1 ]
Slater, Brian
Calhoun, Frank
Liu, Desheng [2 ,3 ]
Van Meirvenne, Marc [4 ]
机构
[1] Ohio State Univ, Carbon Management & Sequestrat Ctr, Sch Environm & Nat Resources, Columbus, OH 43210 USA
[2] Ohio State Univ, Dept Geog, Columbus, OH 43210 USA
[3] Ohio State Univ, Dept Stat, Columbus, OH 43210 USA
[4] Univ Ghent, Dep Soil Management & Soil Care, B-9000 Ghent, Belgium
关键词
SPATIAL PREDICTION; SEQUESTRATION; PATTERNS; TEXTURE; CLIMATE; MATTER; POOLS; BULK;
D O I
10.2136/sssaj2007.0410
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The objective of this study was to predict and map SOC stocks at different depth intervals within the upper I-in depth using profile depth distribution functions and ordinary kriging. These approaches were tested for the state of Indiana as a case study. A total of 464 pedons representing 204 soil series was obtained from the National Soil Survey Center database. Another 48 soil profile samples were collected to better represent the heterogeneity of the environmental variables. Two methods were used to model the depth distribution of the SOC stocks using negative exponential profile depth functions. In Procedure A, the functions to describe the depth distribution of volumetric C content for each soil profile were fitted using nonlinear least squares. In Procedure B, the exponential functions were fitted to describe the depth distribution of the cumulative SOC stocks. The parameters of the functions were interpolated for the entire study area using ordinary kriging on 81% of the data points (n = 414). The integral of the exponential function up to the desired depth was used to predict SOC stocks within the 0- to 1-, 0- to 0.5-, and 0.5- to 1-m depth intervals. These estimates were validated using the remaining 19% (n = 98) of the data. Procedure B showed a higher prediction accuracy for all depths, with higher rand lower RMSE values. The highest prediction accuracy (r = 0.75, RMSE = 2.89 kg m(-2)) was obtained for SOC stocks in the 0- to 0.5-m depth interval. Using Procedure B, SOC stocks within the top 1 m of Indiana soils were estimated to be 0.90 Pg C.
引用
收藏
页码:614 / 621
页数:8
相关论文
共 44 条
[21]   A multiple regression approach to assess the spatial distribution of Soil Organic Carbon (SOC) at the regional scale (Flanders, Belgium) [J].
Meersmans, J. ;
De Ridder, F. ;
Canters, F. ;
De Baets, S. ;
Van Molle, M. .
GEODERMA, 2008, 143 (1-2) :1-13
[22]   Soil organic carbon stocks in Flemish grasslands: how accurate are they? [J].
Mestdagh, I ;
Lootens, P ;
Van Cleemput, O ;
Carlier, L .
GRASS AND FORAGE SCIENCE, 2004, 59 (04) :310-317
[23]   Prediction and digital mapping of soil carbon storage in the Lower Namoi Valley [J].
Minasny, B ;
McBratney, AB ;
Mendonça-Santos, ML ;
Odeh, IOA ;
Guyon, B .
AUSTRALIAN JOURNAL OF SOIL RESEARCH, 2006, 44 (03) :233-244
[24]  
MORAN PAP, 1950, BIOMETRIKA, V37, P17, DOI 10.2307/2332142
[25]  
*MULT LAND CHAR CO, 2006, NAT LAND COV DAT 200
[26]  
National Soil Survey Laboratory, 2006, SOIL CHAR DAT
[27]  
Nelson D.W., 1996, Total Carbon, P961, DOI DOI 10.2136/SSSABOOKSER5.3.C34
[28]   SPATIAL PREDICTION OF SOIL PROPERTIES FROM LANDFORM ATTRIBUTES DERIVED FROM A DIGITAL ELEVATION MODEL [J].
ODEH, IOA ;
MCBRATNEY, AB ;
CHITTLEBOROUGH, DJ .
GEODERMA, 1994, 63 (3-4) :197-214
[29]   Soil carbon sequestration and land-use change: processes and potential [J].
Post, WM ;
Kwon, KC .
GLOBAL CHANGE BIOLOGY, 2000, 6 (03) :317-327
[30]  
POST WM, 1990, AM SCI, V78, P310