Revision Date: February 27, 2009
The results of the analysis of soil chemical parameters, texture, and color are reported for 185 georeferenced soil profile sample points over four forested headwater catchments near Juruena, Mato Grosso, Brazil (Novaes Filho et al., 2007a and Novaes Filho et al., 2007b). Samples were collected from an approximately 20 x 20-m grid over each watershed from 2004/05/01 to 2004/08/18. By sampling each location at depths of 0-20 and 40-60 cm it was possible to distinguish and map the principle soil classes found in the study area to the 2nd category level of the Brazilian System of Soil Classification (Cooper et al., 2005) associated with the topographic relief.
The data set contains one comma separated ASCII data file with spatially referenced soil nutrient and organic carbon data from 0-20 cm (A layer, topsoil) and 40-60 cm (B layer, subsoil) depths for the Juruena watersheds study area.
A satisfactory relationship between the redness index of the diagnostic horizons and the soil class colors was also found. In spite of the apparent homogeneity of the visible landscape characteristics such as slope, soil color, and vegetation, the carbon and soil clay attributes were found to vary greatly. This variability over small distances demonstrates that extrapolation of soil characteristics and soil carbon stocks to larger areas could produce erroneous results if the spatial variability of the soil attributes is not taken into consideration.
Figure 1. Soil sample locations (plotted by ORNL DAAC) are depicted with watershed delimitation and streams overlain on a 2002 IKONOS panchromatic image of the forested study location (courtesy of EOS-Webster). Watersheds are identified as B1, B2, B3, and B4 from right to left.
Cite this data set as follows:
Novaes Filho, J.P., E.C. Selva ,E.G. Couto, J. Lehmann, M.S. Johnson, and S.J. Riha. 2009. LBA-ECO ND-11 Soil Properties of Forested Headwater Catchments, Mato Grosso, Brazil. Data set. Available on-line [http://daac.ornl.gov] from Oak Ridge National Laboratory Distributed Active Archive Center, Oak Ridge, Tennessee, U.S.A. doi:10.3334/ORNLDAAC/914
The LBA Data and Publication Policy [http://daac.ornl.gov/LBA/lba_data_policy.html] is in effect for a period of five (5) years from the date of archiving and should be followed by data users who have obtained LBA data sets from the ORNL DAAC. Users who download LBA data in the five years after data have been archived must contact the investigators who collected the data, per provisions 6 and 7 in the Policy.
This data set was archived in March of 2009. Users who download the data between March 2009 and February 2014 must comply with the LBA Data and Publication Policy.
Data users should use the Investigator contact information in this document to communicate with the data provider. Alternatively, the LBA Web Site[http://lba.inpa.gov.br/lba/] in Brazil have current contact information.
Data users should use the Data Set Citation and other applicable references provided in this document to acknowledge use of the data.
Project: LBA (Large-Scale Biosphere-Atmosphere Experiment in the Amazon)
Activity: LBA-ECO
LBA Science Component: Nutrient Dynamics
Team ID: ND-11 (Lehmann/Passos/Couto)
The investigators were Novaes Filho Joao Paulo; Johnson, Mark Stephen; Couto, Eduardo Guimaraes and Lehmann, Johannes. You may contact Novaes Filho, Joao Paulo (jpnovaes@terra.com.br).
LBA Data Set Inventory ID: ND11_Soil_Spatial_Variability
The results of the analysis of soil chemical parameters, texture, and color are reported for 185 georeferenced soil profile sample points over four forested headwater catchments near Juruena, Mato Grosso, Brazil (Novaes Filho, et al., 2007a and Novaes Filho, et al., 2007b). Samples were collected from an approximately 20 x 20-m grid over each watershed from 2004/05/01 to 2004/08/18. By sampling each location at depths of 0-20 and 40-60 cm it was possible to distinguish and map the principle soil classes found in the study area to the 2nd category level of the Brazilian System of Soil Classification (Cooper et al., 2005) associated with the topographic relief.
The data set contains one comma separated ASCII data file with spatially referenced soil nutrient and organic carbon data from 0-20 cm (A layer, topsoil) and 40-60 cm (B layer, subsoil) depths for the Juruena watersheds study area.
A satisfactory relationship between the redness index of the diagnostic horizons and the soil class colors was also found. In spite of the apparent homogeneity of the visible landscape characteristics such as slope, soil color, and vegetation, the carbon and soil clay attributes were found to vary greatly. This variability over small distances demonstrates that extrapolation of soil characteristics and soil carbon stocks to larger areas could produce erroneous results if the spatial variability of the soil attributes is not taken into consideration.
Data set contains spatially referenced soil nutrient and carbon data for 0-20 cm and 40-60 cm depths for Juruena watersheds study area.
Related Data Sets:
LBA-ECO ND-11 Coarse Particulate Organic Carbon Watershed Exports, Jurena: 2003-2004
LBA-ECO ND-11 Stream Carbon and Nutrients, Mato Grosso, Brazil: 2003-2006
One comma-delimited ASCII file is provided. Values of -9999 in the ASCII file indicate missing values.
Juruena_basins_soils.csv
COLUMN | COLUMN HEADING | DESCRIPTION |
---|---|---|
1 | UTMX | sample location, latitude coordinate for Universal Transverse Mercator (UTM) zone 21S (easting) |
2 | UTMY | sample location, longitude coordinate for UTM zone 21S (northing) |
3 | pH_H2O_0_20 | soil pH in water, 1: 2.5 w/v slurry, 0-20 cm depth |
4 | pH_CaCl2_0_20 | soil pH in 0.01 M CaCl2 solution, 1;2.5 w/v slurry, 0-20 cm depth |
5 | P_0_20 | soil phosphorus (mg/dm3), 0-20 cm depth |
6 | K_0_20 | soil potassium (mg/dm3), 0-20 cm depth |
7 | Ca_0_20 | soil calcium (cmolc/dm3), 0-20 cm depth |
8 | Mg_0_20 | soil magnesium (cmolc/dm3), 0-20 cm depth |
9 | Al_0_20 | soil aluminum (cmolc/dm3), 0-20 cm depth |
10 | H_0_20 | soil hydronium (cmolc/dm3), 0-20 cm depth |
11 | Clay_pct_0_20 | soil clay content (%), 0-20 cm depth |
12 | Silt_pct_0_20 | soil silt content (%), 0-20 cm depth |
13 | Sand_pct_0_20 | soil sand content (%), 0-20 cm depth |
14 | SumCat_0_20 | sum of base cations (cmolc/dm3), 0-20 cm depth |
15 | CEC_0_20 | cation exchange capacity (cmolc/dm3), 0-20 cm depth |
16 | Sat_Bas_0_20 | base saturation of cation exchange capacity (%), 0-20 cm depth |
17 | Al_Sat_0_20 | aluminum saturation (%), 0-20 cm depth |
18 | C_Tot_0_20 | soil total carbon (g/kg), 0-20 cm depth |
19 | Color_0_20 | soil color, Munsell color notation, 0-20 cm depth |
20 | pH_H2O_40_60 | soil pH in water, 1: 2.5 w/v slurry, 40-60 cm depth |
21 | pH_CaCl2_40_60 | soil pH in 0.01 M CaCl2 solution, 1;2.5 w/v slurry, 40-60 cm depth |
22 | P_40_60 | soil phosphorus (mg/dm3), 40-60 cm depth |
23 | K_40_60 | soil potassium (mg/dm3), 40-60 cm depth |
24 | Ca_plus_Mg_40_60 | sum of soil calcium and magnesium (cmolc/dm3), 40-60 cm depth |
25 | Al_40_60 | soil aluminum (cmolc/dm3), 40-60 cm depth |
26 | H_40_60 | soil hydronium (cmolc/dm3), 40-60 cm depth |
27 | Clay_pct_40_60 | soil clay content (%), 40-60 cm depth |
28 | Silt_pct_40_60 | soil silt content (%), 40-60 cm depth |
29 | Sand_pct_40_60 | soil sand content (%), 40-60 cm depth |
30 | SumCat_40_60 | sum of base cations (cmolc/dm3), 40-60 cm depth |
31 | CEC_40_60 | cation exchange capacity (cmolc/dm3), 40-60 cm depth |
32 | Sat_Bas_40_60 | base saturation of cation exchange capacity (%), 40-60 cm depth |
33 | Al_Sat_40_60 | aluminum saturation (%), 40-60 cm depth |
34 | C_Tot_40_60 | soil total carbon (g/kg), 40-60 cm depth |
35 | Color_40_60 | soil color, Munsell color notation, 40-60 cm depth |
Example Data Records:
UTMX,UTMY,pH_H2O_0_20,pH_CaCl2_0_20,P_0_20,K_0_20,Ca_0_20,Mg_0_20,Al_0_20,H_0_20,Clay_pct_0_20, Silt_pct_0_20,Sand_pct_0_20,SumCat_0_20,CEC_0_20,Sat_Bas_0_20,Al_Sat_0_20,C_Tot_0_20,Color_0_20, pH_H2O_40_60,pH_CaCl2_40_60,P_40_60,K_40_60,Ca_plus_Mg_40_60,Al_40_60,H_40_60,Clay_pct_40_60,Silt_pct_40_60, Sand_pct_40_60,SumCat_40_60,CEC_40_60,Sat_Bas_40_60,Al_Sat_40_60,C_Tot_40_60,Color_40_60,,,,,, 339525,8841537,4.5,4.0,1.1,38,0.6,0.3,0.8,2.9,18.2, 6.1,75.7,1.0,4.7,21.2,44.5,8.92,5YR 4/6, 4.4,4.1,0.3,4,0.3,0.4,2.3,33.3,0.9, 65.7,0.3,3.0,10.3,56.3,5.72,"2,5YR 4/6",,,,,, 339510,8841550,4.2,3.7,0.6,52,0.3,0.2,1.3,2.4,27.5, 2.1,70.4,0.6,4.3,14.6,66.7,8.62,5YR 4/6, 4.2,3.9,0.4,10,0.3,0.4,2.7,30.2,1.0, 68.9,0.3,3.4,9.6,55.1,6.10,"2,5YR 4/6",,,,,, 339142,8841453,4.9,4.3,1.7,142,1.1,1.0,0.1,4.2,50.5, 18.6,30.9,2.5,6.8,36.4,4.8,14.81,5YR 5/6, 4.9,4.3,0.5,24,0.6,0.3,1.3,46.1,13.2, 40.8,0.7,2.2,29.6,31.2,7.39,5YR 6/6,,,,,, Blank lines added to improve readability. |
Site Boundaries: (All latitude and longitude given in decimal degrees)
Site (Region) | Westernmost Longitude | Easternmost Longitude | Northernmost Latitude | Southernmost Latitude | Geodetic Datum |
---|---|---|---|---|---|
Mato Grosso - Juruena ( Mato Grosso) | -58.470796 | -58.466252 | -10.475392 | -10.478216 | World Geodetic System, 1984 (WGS-84) |
Time period:
Platform/Sensor/Parameters measured include:
Data set contains results from field study of spatial variability of soil properties.
No known problems with data.
Soil samples collected using dutch auger and analyzed using EMBRAPA standard methods (Brazilian Agricultural Research Corporation) for analysis of soil chemical and physical properties (Silva et al., 1998). The units of cmolc (centimoles of charge) and dm3 (cubic decimeters) are common in Brazilian soil analyses employing EMBRAPA standards.
Soil
texture was determined using the pipette method with 16 hours of slow
shaking (30 rpm) and dispersion of organic matter with NaOH and sodium
hexametaphosphate.
Soil color was determined on fresh, moist soils in the field using a
Munsell color chart.
Exchangeable calcium, magnesium and aluminum were all determined on dry
soils extracted with 1 M KCl. Aluminum concentrations were
measured via titration with NaOH. Calcium and magnesium concentrations
were determined by titration with EDTA (provides a value for the
concentration of Ca + Mg). Concentration of exchangeable Ca alone was
determined by titrating the 1M KCl extract with 0.0125M EDTA after
addition of calcon carbonic acid. Exchangeable Mg
concentrations are then determined as the difference between Ca + Mg
and Ca concentrations.
Available phosphorus, exchangeable potassium and sodium were all
extracted from air dry soils using a Melich I extraction solution (0.05
M HCl + 0.0125 M H2SO4). The ratio of soil to extraction
solution was 1:10 w/v. Phosphorus in the extractant solution
was measured on a spectrophotometer using the ascorbic acid- molybdate
blue reaction. Potassium and sodium were measured by flame
photometry (atomic absorbtion).
Potential acidity, the sum of aluminum and hydrogen ion concentrations
extracted with 0.5M calcium acetate solution was measured by titration
with 0.025M NaOH phenolphthalein as an indicator.
The analysis of carbon
was done using the combustion method at high temperatures (Eltra oven
at 1350 degrees C) and an elemental analyzer (Multi NC 3000) in which
all forms of carbon in the soil are converted to CO2 followed by
measurement of the CO2 (total carbon), following the method described
by the Soil Survey Staff (1996).
Equations for calculated values:
Total exchangeable bases
(S) = (Ca2+) + ( Mg2+) + ( K+) + (Na+)
Cation exchange capacity (T) = S + (H+) + (Al3+)
Base saturation (V) = 100*(S/T)
Exchangeable Al saturation (m) = 100*( (Al3+)/(S + Al3+))
This data set is available through the Oak Ridge National Laboratory (ORNL) Distributed Active Archive Center (DAAC).
E-mail:
uso@daac.ornl.gov
Telephone: +1 (865) 241-3952
Cooper M, Mendes LMS, Silva WLC, Sparovek G. 2005. A national soil profile database for Brazil available to international scientists. Soil Science Society of America Journal 69: 649-652. The database is available for free download at http://www.esalq.usp.br/gerd/ (verified 04 Feb 2008).
Novaes Filho J.P., Couto E.G., de Oliveira V.A., Johnson M.S., Lehmann J., Riha J. (2007a). Spatial variability of soil physical attributes used in soil classification of microbasins in southern Amazonia. Revista Brasileira de Ciencia do Solo (Brazilian Journal of Soil Science), 31, 91-100.doi:10.1590/S0100-06832007000100010.
Novaes filho J.P., Selva E.C., Couto, E.G., Lehmann, J., Johnson, M.S., Riha S.J. (2007b) Spatial distribution of soil carbon under primary forest cover in Southern amazonia. Revista Arvore (Tree Journal), 31, 83-92.
Silva, F.C. da, P.A. da Eira, W. De Oliveira Barreto, D. Vidal Perez and C.A. Silva. 1998. Analises químicas para avaliacao da fertilidade do solo: Metodos usados na Embrapa Solos. Doc. No. 3
Soil Survey Staff. 1996. Soil survey laboratory methods manual. Soil Survey Investigations, Report 42 (Version 3.0). U.S. Department of Agriculture, Natural Resources Conservation Service, National Soil Survey Center, Lincoln, NE. 693 p.