Soil organic carbon mapping and prediction based on depth intervals using kriging technique: A case of study in alluvial soil from Sudan

Soil organic carbon plays a vital role in the arid and semiarid regions. This study aimed to predict and map soil organic carbon content at soil depth intervals of 0-0.3 m, 0.3-0.6 m, 0.6-0.9 m, and 0.9-1.2 m in alluvium soils along Blue Nile and River Nile, Sudan. Ordinary kriging (OK) technique wa...

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Main Authors: Magboul M. Sulieman, Abdallah M. AlGarni
Format: Article
Language:English
Published: Federation of Eurasian Soil Science Societies 2019-01-01
Series:Eurasian Journal of Soil Science
Subjects:
Online Access:http://ejss.fesss.org/10.18393/ejss.492466
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spelling doaj-df65bb7a9bd148e18a344f34e6133f1d2020-11-25T00:29:27ZengFederation of Eurasian Soil Science SocietiesEurasian Journal of Soil Science 2147-42492147-42492019-01-0181445310.18393/ejss.492466Soil organic carbon mapping and prediction based on depth intervals using kriging technique: A case of study in alluvial soil from SudanMagboul M. Sulieman0Abdallah M. AlGarni1Department of Soil and Environment Sciences, Faculty of Agriculture, University of Khartoum, Khartoum, SudanInstitute of Environmental Studies, University of Khartoum, Khartoum, SudanSoil organic carbon plays a vital role in the arid and semiarid regions. This study aimed to predict and map soil organic carbon content at soil depth intervals of 0-0.3 m, 0.3-0.6 m, 0.6-0.9 m, and 0.9-1.2 m in alluvium soils along Blue Nile and River Nile, Sudan. Ordinary kriging (OK) technique was used as a geostatistical tool and applied to model the spatial variability of soil organic carbon in the study area. A total of 38 soil profiles were excavated in the study area and 152 samples from the four depths intervals were collected for determining organic carbon content. Results revealed that, the spatial autocorrelation for the different soil layers was moderate to weak with a nugget to sill ratios ranging from 0.21 to 0.86 suggesting their controlled by both intrinsic and extrinsic factors. The root mean square error standardized (RMSE) of the predictions ranging from 0.79 to 0.83 indicating that the model which generated by ordinary kriging was correctly estimating the variability of soil organic carbon in the study area. http://ejss.fesss.org/10.18393/ejss.492466Alluvial soilspatial autocorrelationsemivariogramsoil organic carbonCokriging
collection DOAJ
language English
format Article
sources DOAJ
author Magboul M. Sulieman
Abdallah M. AlGarni
spellingShingle Magboul M. Sulieman
Abdallah M. AlGarni
Soil organic carbon mapping and prediction based on depth intervals using kriging technique: A case of study in alluvial soil from Sudan
Eurasian Journal of Soil Science
Alluvial soil
spatial autocorrelation
semivariogram
soil organic carbon
Cokriging
author_facet Magboul M. Sulieman
Abdallah M. AlGarni
author_sort Magboul M. Sulieman
title Soil organic carbon mapping and prediction based on depth intervals using kriging technique: A case of study in alluvial soil from Sudan
title_short Soil organic carbon mapping and prediction based on depth intervals using kriging technique: A case of study in alluvial soil from Sudan
title_full Soil organic carbon mapping and prediction based on depth intervals using kriging technique: A case of study in alluvial soil from Sudan
title_fullStr Soil organic carbon mapping and prediction based on depth intervals using kriging technique: A case of study in alluvial soil from Sudan
title_full_unstemmed Soil organic carbon mapping and prediction based on depth intervals using kriging technique: A case of study in alluvial soil from Sudan
title_sort soil organic carbon mapping and prediction based on depth intervals using kriging technique: a case of study in alluvial soil from sudan
publisher Federation of Eurasian Soil Science Societies
series Eurasian Journal of Soil Science
issn 2147-4249
2147-4249
publishDate 2019-01-01
description Soil organic carbon plays a vital role in the arid and semiarid regions. This study aimed to predict and map soil organic carbon content at soil depth intervals of 0-0.3 m, 0.3-0.6 m, 0.6-0.9 m, and 0.9-1.2 m in alluvium soils along Blue Nile and River Nile, Sudan. Ordinary kriging (OK) technique was used as a geostatistical tool and applied to model the spatial variability of soil organic carbon in the study area. A total of 38 soil profiles were excavated in the study area and 152 samples from the four depths intervals were collected for determining organic carbon content. Results revealed that, the spatial autocorrelation for the different soil layers was moderate to weak with a nugget to sill ratios ranging from 0.21 to 0.86 suggesting their controlled by both intrinsic and extrinsic factors. The root mean square error standardized (RMSE) of the predictions ranging from 0.79 to 0.83 indicating that the model which generated by ordinary kriging was correctly estimating the variability of soil organic carbon in the study area.
topic Alluvial soil
spatial autocorrelation
semivariogram
soil organic carbon
Cokriging
url http://ejss.fesss.org/10.18393/ejss.492466
work_keys_str_mv AT magboulmsulieman soilorganiccarbonmappingandpredictionbasedondepthintervalsusingkrigingtechniqueacaseofstudyinalluvialsoilfromsudan
AT abdallahmalgarni soilorganiccarbonmappingandpredictionbasedondepthintervalsusingkrigingtechniqueacaseofstudyinalluvialsoilfromsudan
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