Mapping rootable depth and root zone plant-available water holding capacity of the soil of sub-Saharan Africa
| Autor: | Johan G B, Leenaars, Lieven, Claessens, Gerard B M, Heuvelink, Tom, Hengl, Maria, Ruiperez González, Lenny G J, van Bussel, Nicolas, Guilpart, Haishun, Yang, Kenneth G, Cassman |
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| Rok vydání: | 2018 |
| Předmět: |
pF
logarithm of the negative hydrostatic head or matrix potential RZD root zone depth (rootable depth) ISFM Integrated Soil Fertility Management Rootability Digital soil map Article AfSS Africa Sentinel Sites database RI rootability index BD bulk density PTF pedotransfer function Root zone depth VMC volumetric moisture content Soil data DSM digital soil mapping Soil water EC electrical conductivity SSA sub-Saharan Africa SFEF soil fine earth fraction Sub-Saharan Africa FC field capacity PWP permanent wilting point PAWHC plant-available water holding capacity Maize AfSP Africa Soil Profiles database RZ-PAWHC root zone plant-available water holding capacity CEC cation exchange capacity |
| Zdroj: | Geoderma |
| ISSN: | 0016-7061 |
| Popis: | In rainfed crop production, root zone plant-available water holding capacity (RZ-PAWHC) of the soil has a large influence on crop growth and the yield response to management inputs such as improved seeds and fertilisers. However, data are lacking for this parameter in sub-Saharan Africa (SSA). This study produced the first spatially explicit, coherent and complete maps of the rootable depth and RZ-PAWHC of soil in SSA. We compiled geo-referenced data from 28,000 soil profiles from SSA, which were used as input for digital soil mapping (DSM) techniques to produce soil property maps of SSA. Based on these soil properties, we developed and parameterised (pedotransfer) functions, rules and criteria to evaluate soil water retention at field capacity and wilting point, the soil fine earth fraction from coarse fragments content and, for maize, the soil rootability (relative to threshold values) and rootable depth. Maps of these secondary soil properties were derived using the primary soil property maps as input for the evaluation rules and the results were aggregated over the rootable depth to obtain a map of RZ-PAWHC, with a spatial resolution of 1 km2. The mean RZ-PAWHC for SSA is 74 mm and the associated average root zone depth is 96 cm. Pearson correlation between the two is 0.95. RZ-PAWHC proves most limited by the rootable depth but is also highly sensitive to the definition of field capacity. The total soil volume of SSA potentially rootable by maize is reduced by one third (over 10,500 km3) due to soil conditions restricting root zone depth. Of these, 4800 km3 are due to limited depth of aeration, which is the factor most severely limiting in terms of extent (km2), and 2500 km3 due to sodicity which is most severely limiting in terms of degree (depth in cm). Depth of soil to bedrock reduces the rootable soil volume by 2500 km3, aluminium toxicity by 600 km3, porosity by 120 km3 and alkalinity by 20 km3. The accuracy of the map of rootable depth and thus of RZ-PAWHC could not be validated quantitatively due to absent data on rootability and rootable depth but is limited by the accuracy of the primary soil property maps. The methodological framework is robust and has been operationalised such that the maps can easily be updated as additional data become available. Highlights • Rootable depth & root zone plant-available water holding capacity mapped for SSA • Average rootable depth is 96 cm and associated RZ-PAWHC is 74 mm. • Rootable volume reduced by a third due to restrictive aeration, sodicity, bedrock • Accuracy rootable depth map cannot be validated due to lack of data on rootability. • Robust framework; maps can be updated as extra data become available. |
| Databáze: | OpenAIRE |
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