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Basic Technical Commonly tested

Soil Water Retention Capacity

noun

Pronunciation: /sɔɪl ˈwɔːtər rɪˈtenʃən kəˈpæsɪti/

The ability of soil to hold water against gravitational forces, determined by soil texture, structure, and organic matter content. This parameter directly affects water availability to plant roots during stress periods and depends on pore size distribution.

Plain English

How much water soil can hold and make available to plant roots before it drains away.

Etymology & History

Origin languageLatin, English
Rootsolum (Latin 'ground') + water (English) + retentio (Latin 'holding back') + capacitas (Latin 'able to hold')
First recorded use1930s
Usage frequencyCommon

Usage

"Sandy soils with low water retention capacity required more frequent irrigation to maintain plant growth under drought conditions."

Style guide notes: Report values in volumetric percentage or depth units; specify measurement method for comparability.

Also known as

water holding capacity soil water availability

Contrasted with

drainage rate water permeability

Related Terms

Frequently Asked Questions

How does soil texture affect water retention capacity?

Clay soils retain more water due to smaller pores; sandy soils retain less water but drain faster.

How can soil water retention capacity be improved?

Adding organic matter increases water-holding capacity through improved soil structure and aggregate stability.

Why Test Candidates on This?

Essential for characterizing drought stress severity and designing irrigation strategies in field experiments.

Required skill level: Junior

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