Physical topsoil properties in Murugusi, Western Kenya

General: Lab determined topsoil bulk density, contents of sand, clay and organic carbon in Murugusi, W. Kenya, together with spatial coordinates of where the soil samples were taken (rounded to the closest center point of a 250 m × 250 m raster). All lab analyses were carried out at the ILRI/CIAT la...

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Autores principales: Piikki, Kristin, Söderström, Mats, Sommer, Rolf, Silva, Mayesse Aparecida da
Formato: Conjunto de datos
Lenguaje:Inglés
Publicado: International Center for Tropical Agriculture 2019
Materias:
Acceso en línea:https://hdl.handle.net/10568/102151
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author Piikki, Kristin
Söderström, Mats
Sommer, Rolf
Silva, Mayesse Aparecida da
author_browse Piikki, Kristin
Silva, Mayesse Aparecida da
Sommer, Rolf
Söderström, Mats
author_facet Piikki, Kristin
Söderström, Mats
Sommer, Rolf
Silva, Mayesse Aparecida da
author_sort Piikki, Kristin
collection Repository of Agricultural Research Outputs (CGSpace)
description General: Lab determined topsoil bulk density, contents of sand, clay and organic carbon in Murugusi, W. Kenya, together with spatial coordinates of where the soil samples were taken (rounded to the closest center point of a 250 m × 250 m raster). All lab analyses were carried out at the ILRI/CIAT lab in Nairob, Kenya. Soil sampling: At each sample location, one composite topsoil sample was taken; three cores of 7 cm in diameter taken within an area of one square meter. The soil was taken from 0-0.2 m depth below any organic (O) horizon. Determination of soil properties: The bulk density of the soil was determined by taking two undisturbed soil samples (0-10 cm and 10-20 cm depth) of known volume (100 cm2) and weighting them after air drying. Soil fractions of clay (<0.002 mm) and sand (0.05-2 mm) were determined by the hydrometer method (Estefan et al., 2014), using 10% sodium hexametaphosphate as the dispersing agent. Soil pH was determined potentiometrically on a soil suspension of 1:2 (soil: water). Total carbon was measured after dry combustion using an elemental analyser (Elementar Vario max cube; ISO 10694, first edition 1995-03-01) Reference: Estefan G., Sommer R., Ryan J. (2014) Analytical Methods for Soil-Plant and Water in Dry Areas. A Manual of Relevance to the West Asia and North Africa Region. 3rd Edition, International Center for Agricultural Research in the Dry Areas, Aleppo, 255 pp. Available online at: http://repo.mel.cgiar.org:8080/handle/20.500.11766/7512?show=full. Verified: October 9, 2018. Acknowledgements: We are deeply thankful for the good services provided by John Mukulama (soil sampling), John Yumbya Mutua (soil sampling) and Francis Mungthu Njenga (lab analyses) The project was carried out within the CGIAR Research Program on Water, Land and Ecosystems (WLE).
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spelling CGSpace1021512025-03-13T09:45:58Z Physical topsoil properties in Murugusi, Western Kenya Piikki, Kristin Söderström, Mats Sommer, Rolf Silva, Mayesse Aparecida da soil soil organic matter sand General: Lab determined topsoil bulk density, contents of sand, clay and organic carbon in Murugusi, W. Kenya, together with spatial coordinates of where the soil samples were taken (rounded to the closest center point of a 250 m × 250 m raster). All lab analyses were carried out at the ILRI/CIAT lab in Nairob, Kenya. Soil sampling: At each sample location, one composite topsoil sample was taken; three cores of 7 cm in diameter taken within an area of one square meter. The soil was taken from 0-0.2 m depth below any organic (O) horizon. Determination of soil properties: The bulk density of the soil was determined by taking two undisturbed soil samples (0-10 cm and 10-20 cm depth) of known volume (100 cm2) and weighting them after air drying. Soil fractions of clay (<0.002 mm) and sand (0.05-2 mm) were determined by the hydrometer method (Estefan et al., 2014), using 10% sodium hexametaphosphate as the dispersing agent. Soil pH was determined potentiometrically on a soil suspension of 1:2 (soil: water). Total carbon was measured after dry combustion using an elemental analyser (Elementar Vario max cube; ISO 10694, first edition 1995-03-01) Reference: Estefan G., Sommer R., Ryan J. (2014) Analytical Methods for Soil-Plant and Water in Dry Areas. A Manual of Relevance to the West Asia and North Africa Region. 3rd Edition, International Center for Agricultural Research in the Dry Areas, Aleppo, 255 pp. Available online at: http://repo.mel.cgiar.org:8080/handle/20.500.11766/7512?show=full. Verified: October 9, 2018. Acknowledgements: We are deeply thankful for the good services provided by John Mukulama (soil sampling), John Yumbya Mutua (soil sampling) and Francis Mungthu Njenga (lab analyses) The project was carried out within the CGIAR Research Program on Water, Land and Ecosystems (WLE). 2019-07-02 2019-07-10T15:46:43Z 2019-07-10T15:46:43Z Dataset https://hdl.handle.net/10568/102151 en https://hdl.handle.net/10568/98859 Open Access International Center for Tropical Agriculture Piikki, Kristin; Söderström, Mats; Sommer, Rolf; Da Silva, Mayesse, 2019, "Physical topsoil properties in Murugusi, Western Kenya", https://doi.org/10.7910/DVN/GVNJAB, Harvard Dataverse, V1, UNF:6:Lxx21ICZO4yG59/xN+m8WQ== [fileUNF]
spellingShingle soil
soil organic matter
sand
Piikki, Kristin
Söderström, Mats
Sommer, Rolf
Silva, Mayesse Aparecida da
Physical topsoil properties in Murugusi, Western Kenya
title Physical topsoil properties in Murugusi, Western Kenya
title_full Physical topsoil properties in Murugusi, Western Kenya
title_fullStr Physical topsoil properties in Murugusi, Western Kenya
title_full_unstemmed Physical topsoil properties in Murugusi, Western Kenya
title_short Physical topsoil properties in Murugusi, Western Kenya
title_sort physical topsoil properties in murugusi western kenya
topic soil
soil organic matter
sand
url https://hdl.handle.net/10568/102151
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