Soil organic carbon stock in kg/m2 for 5 standard depth intervals (0–10, 10–30, 30–60, 60–100 and 100–200 cm) at 250 m resolution

Soil organic carbon stock in kg/m2 for 5 standard depth intervals (0–10, 10–30, 30–60, 60–100 and 100–200 cm) at 250 m resolution. To convert to t/ha multiply by 10. Derived using soil organic carbon content (https://doi.org/10.5281/zenodo.1475457), bulk density (https://doi.org/10.5281/zenodo.14759...

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Bibliographic Details
Main Authors: Tomislav Hengl, Ichsani Wheeler
Format: Dataset
Language:English
Published: 2018
Subjects:
Online Access:https://zenodo.org/record/2536040
https://doi.org/10.5281/zenodo.2536040
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record_format openpolar
spelling ftzenodo:oai:zenodo.org:2536040 2023-05-15T13:52:16+02:00 Soil organic carbon stock in kg/m2 for 5 standard depth intervals (0–10, 10–30, 30–60, 60–100 and 100–200 cm) at 250 m resolution Tomislav Hengl Ichsani Wheeler 2018-12-24 https://zenodo.org/record/2536040 https://doi.org/10.5281/zenodo.2536040 eng eng doi:10.5281/zenodo.1475453 https://zenodo.org/communities/zenodo https://zenodo.org/record/2536040 https://doi.org/10.5281/zenodo.2536040 oai:zenodo.org:2536040 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-sa/4.0/legalcode LandGIS soil carbon info:eu-repo/semantics/other dataset 2018 ftzenodo https://doi.org/10.5281/zenodo.253604010.5281/zenodo.1475453 2023-03-11T03:56:25Z Soil organic carbon stock in kg/m2 for 5 standard depth intervals (0–10, 10–30, 30–60, 60–100 and 100–200 cm) at 250 m resolution. To convert to t/ha multiply by 10. Derived using soil organic carbon content (https://doi.org/10.5281/zenodo.1475457), bulk density (https://doi.org/10.5281/zenodo.1475970) and coarse fragments (https://doi.org/10.5281/zenodo.2525681), predicted from point data at 6 standard depths. Depth to bed rock has been ignored, hence total stocks might be about 10–15% lower then reported. Processing steps are described in detail here. Antarctica is not included. To access and visualize maps use: https://openlandmap.org If you discover a bug, artifact or inconsistency in the maps, or if you have a question please use some of the following channels: Technical issues and questions about the code: https://gitlab.com/openlandmap/global-layers/issues General questions and comments: https://disqus.com/home/forums/landgis/ All files internally compressed using "COMPRESS=DEFLATE" creation option in GDAL. File naming convention: sol = theme: soil, organic.carbon.stock = variable: soil organic carbon stock in kg/m2, msa.kgm2 = determination method: derived from organic carbon content, bulk density and coarse fragments, m = mean value, 250m = spatial resolution / block support: 250 m, b0.10cm = vertical reference: 0-10 cm layer below surface, 1950.2017 = time reference: period 1950-2017, v0.2 = version number: 0.2 Dataset Antarc* Antarctica Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic LandGIS
soil carbon
spellingShingle LandGIS
soil carbon
Tomislav Hengl
Ichsani Wheeler
Soil organic carbon stock in kg/m2 for 5 standard depth intervals (0–10, 10–30, 30–60, 60–100 and 100–200 cm) at 250 m resolution
topic_facet LandGIS
soil carbon
description Soil organic carbon stock in kg/m2 for 5 standard depth intervals (0–10, 10–30, 30–60, 60–100 and 100–200 cm) at 250 m resolution. To convert to t/ha multiply by 10. Derived using soil organic carbon content (https://doi.org/10.5281/zenodo.1475457), bulk density (https://doi.org/10.5281/zenodo.1475970) and coarse fragments (https://doi.org/10.5281/zenodo.2525681), predicted from point data at 6 standard depths. Depth to bed rock has been ignored, hence total stocks might be about 10–15% lower then reported. Processing steps are described in detail here. Antarctica is not included. To access and visualize maps use: https://openlandmap.org If you discover a bug, artifact or inconsistency in the maps, or if you have a question please use some of the following channels: Technical issues and questions about the code: https://gitlab.com/openlandmap/global-layers/issues General questions and comments: https://disqus.com/home/forums/landgis/ All files internally compressed using "COMPRESS=DEFLATE" creation option in GDAL. File naming convention: sol = theme: soil, organic.carbon.stock = variable: soil organic carbon stock in kg/m2, msa.kgm2 = determination method: derived from organic carbon content, bulk density and coarse fragments, m = mean value, 250m = spatial resolution / block support: 250 m, b0.10cm = vertical reference: 0-10 cm layer below surface, 1950.2017 = time reference: period 1950-2017, v0.2 = version number: 0.2
format Dataset
author Tomislav Hengl
Ichsani Wheeler
author_facet Tomislav Hengl
Ichsani Wheeler
author_sort Tomislav Hengl
title Soil organic carbon stock in kg/m2 for 5 standard depth intervals (0–10, 10–30, 30–60, 60–100 and 100–200 cm) at 250 m resolution
title_short Soil organic carbon stock in kg/m2 for 5 standard depth intervals (0–10, 10–30, 30–60, 60–100 and 100–200 cm) at 250 m resolution
title_full Soil organic carbon stock in kg/m2 for 5 standard depth intervals (0–10, 10–30, 30–60, 60–100 and 100–200 cm) at 250 m resolution
title_fullStr Soil organic carbon stock in kg/m2 for 5 standard depth intervals (0–10, 10–30, 30–60, 60–100 and 100–200 cm) at 250 m resolution
title_full_unstemmed Soil organic carbon stock in kg/m2 for 5 standard depth intervals (0–10, 10–30, 30–60, 60–100 and 100–200 cm) at 250 m resolution
title_sort soil organic carbon stock in kg/m2 for 5 standard depth intervals (0–10, 10–30, 30–60, 60–100 and 100–200 cm) at 250 m resolution
publishDate 2018
url https://zenodo.org/record/2536040
https://doi.org/10.5281/zenodo.2536040
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_relation doi:10.5281/zenodo.1475453
https://zenodo.org/communities/zenodo
https://zenodo.org/record/2536040
https://doi.org/10.5281/zenodo.2536040
oai:zenodo.org:2536040
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-sa/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.253604010.5281/zenodo.1475453
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