Système d'information stratégique et agriculture (serveur d'exploration)

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Exploring land quality effects on world food supply

Identifieur interne : 000722 ( Istex/Corpus ); précédent : 000721; suivant : 000723

Exploring land quality effects on world food supply

Auteurs : J. Bouma ; N. H Batjes ; J. J. R Groot

Source :

RBID : ISTEX:57030A2AF7924B4F8F6BE2425309F8753879C02F

Abstract

In a previous study, simulations of agricultural production potentials were made for different exploratory scenarios considering population growth, type of diet and low and high input agriculture. Results indicated that future world populations can be fed, but problems are likely in South Asia. The simulations involved gross generalizations for soil conditions. For example, possible effects of soil degradation were not expressed. The current study was made to explore the effects of the different types of soil degradation on agricultural production, using major soil groupings of the Humid Tropics and Seasonally Dry (Sub)Tropics as examples. Degradation (compaction, erosion and acidification) is expressed in terms of soil quality indicators relating potential to actual production. Results are characteristically different for different soil units (genoforms), and the suggestion is made to present such differences in future soil databases for phenoforms that express effects of different forms of degradation or improvement, allowing better assessments for exploratory land use scenarios. Field studies should be initiated to describe realistic phenoforms for any given genoform.

Url:
DOI: 10.1016/S0016-7061(98)00034-2

Links to Exploration step

ISTEX:57030A2AF7924B4F8F6BE2425309F8753879C02F

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<abstract lang="en">In a previous study, simulations of agricultural production potentials were made for different exploratory scenarios considering population growth, type of diet and low and high input agriculture. Results indicated that future world populations can be fed, but problems are likely in South Asia. The simulations involved gross generalizations for soil conditions. For example, possible effects of soil degradation were not expressed. The current study was made to explore the effects of the different types of soil degradation on agricultural production, using major soil groupings of the Humid Tropics and Seasonally Dry (Sub)Tropics as examples. Degradation (compaction, erosion and acidification) is expressed in terms of soil quality indicators relating potential to actual production. Results are characteristically different for different soil units (genoforms), and the suggestion is made to present such differences in future soil databases for phenoforms that express effects of different forms of degradation or improvement, allowing better assessments for exploratory land use scenarios. Field studies should be initiated to describe realistic phenoforms for any given genoform.</abstract>
<note type="footnote">Invited paper for the Symposium: Global Carrying Capacity: Feeding the People of the 21st Century, held at the 89th Annual Meetings of the American Society of Agronomy in Anaheim, CA, USA. The symposium was sponsored by the Divisions: S-5, A-3, A-5, A-6, C-3, S-4, S-6 and S-11.</note>
<note type="content">Fig. 1: Climate diagrams showing the monthly distribution of air temperature (°C), radiation and precipitation (mm).</note>
<note type="content">Fig. 2: Potential and water-limited yield for the genoform and attainable yields for 3 phenoforms (compaction, erosion and liming), by soil type (C4 crop).</note>
<note type="content">Fig. 3: Relative soil quality indicators by soil type (C4 crop; expressed as 100×yieldi/potential yield, where i is water-limited, compaction, erosion and liming, respectively).</note>
<note type="content">Fig. 4: Absolute soil quality indicator by soil type (expressed as 100×water-limited yield/MPY, where MPY is Maximum Potential Yield of C4 crop in the world: 41.4 t−1 dry matter−1 ha−1 yr−1=100%).</note>
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<note type="content">Table 2: Characterisation of agro-ecological zones</note>
<note type="content">Table 3: Main soil units considered by agro-ecological zone</note>
<note type="content">Table 4: Soil parameter values for the genoform and 3 phenoforms</note>
<subject>
<genre>Keywords</genre>
<topic>simulation modelling</topic>
<topic>soil degradation</topic>
<topic>population growth</topic>
</subject>
<relatedItem type="host">
<titleInfo>
<title>Geoderma</title>
</titleInfo>
<titleInfo type="abbreviated">
<title>GEODER</title>
</titleInfo>
<genre type="journal">journal</genre>
<originInfo>
<dateIssued encoding="w3cdtf">199810</dateIssued>
</originInfo>
<identifier type="ISSN">0016-7061</identifier>
<identifier type="PII">S0016-7061(00)X0045-6</identifier>
<part>
<date>199810</date>
<detail type="volume">
<number>86</number>
<caption>vol.</caption>
</detail>
<detail type="issue">
<number>1–2</number>
<caption>no.</caption>
</detail>
<extent unit="issue pages">
<start>1</start>
<end>158</end>
</extent>
<extent unit="pages">
<start>43</start>
<end>59</end>
</extent>
</part>
</relatedItem>
<identifier type="istex">57030A2AF7924B4F8F6BE2425309F8753879C02F</identifier>
<identifier type="DOI">10.1016/S0016-7061(98)00034-2</identifier>
<identifier type="PII">S0016-7061(98)00034-2</identifier>
<accessCondition type="use and reproduction" contentType="copyright">©1998 Elsevier Science B.V.</accessCondition>
<recordInfo>
<recordContentSource>ELSEVIER</recordContentSource>
<recordOrigin>Elsevier Science B.V., ©1998</recordOrigin>
</recordInfo>
</mods>
</metadata>
<serie></serie>
</istex>
</record>

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