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Field Guide of Discovery-based Exercises for - Aseanipm ...

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Section 3 • Living Soil, Integrated Soil Nutrient and Crop Managements<br />

Exercise No. 3.06 55<br />

SOIL WATER HOLDING CAPACITY DETERMINATION:<br />

A SOIL MANAGEMENT GUIDE FOR IMPROVING<br />

PRODUCTIVITY IN GROWING ORGANIC VEGETABLES<br />

BaCKGroUND aND raTIoNalE<br />

Organic matter functions as a ‘granulator’ <strong>of</strong> mineral<br />

particles, being largely responsible <strong>for</strong> loose, easily managed<br />

condition <strong>of</strong> productive soils. Through its effect on physical<br />

condition <strong>of</strong> soils, organic matter also increases amount <strong>of</strong><br />

water a soil can hold or water holding capacity and proportion<br />

<strong>of</strong> this water available <strong>for</strong> plant growth. Soils high in organic<br />

matter are darker and have greater water holding capacity<br />

than soils low in organic matter 56 .<br />

Two major concepts concerning soil water emphasize significance <strong>of</strong> this component <strong>of</strong> soil in<br />

relation to plant growth, namely: (1) water is held within soil spaces (pores) with varying degrees <strong>of</strong><br />

attraction (tenacity) depending on amount <strong>of</strong> water present and size <strong>of</strong> pores; and (2) together with<br />

its dissolved nutrients (salts), soil water makes up soil solution, which is very important as a medium<br />

<strong>for</strong> supplying nutrients to growing plants.<br />

A clearly important characteristic <strong>of</strong> a soil is its ability to hold water. One problem with a coarse<br />

sandy soil is that water (and nutrients) is rapidly lost from soil. One important quality <strong>of</strong> soil organic<br />

matter is that it helps in water retention. To demonstrate this to farmers is a simple exercise that<br />

should help promote use <strong>of</strong> compost and mulch in organic vegetable production. In FFSs, relevant<br />

experiences on water holding capacities <strong>of</strong> different soils can be shared freely among farmers and<br />

facilitators to improve current soil management practices in organic vegetable production. This<br />

particular exercise was designed to address this concern.<br />

How long will this exercise take?<br />

• Thirty minutes to one hour <strong>for</strong> field walks and observations <strong>of</strong> water holding capacities <strong>of</strong> soils<br />

in adjoining and learning fields; and<br />

• Thirty minutes to one hour hands-on and brainstorming session in processing area.<br />

55 Adapted from Callo, Jr., D.P., L.B. Te<strong>of</strong>ilo, and H.A. Tauli (eds). 2002. <strong>Field</strong> <strong>Guide</strong> <strong>of</strong> <strong>Discovery</strong>-<strong>based</strong> <strong>Exercises</strong> <strong>for</strong> Vegetable IPM, Volume II. SEAMEO<br />

Regional Center <strong>for</strong> Graduate Study and Research in Agriculture (SEARCA), Los Baños, Laguna, Philippines. pp72-75.<br />

56 Brady, N.C. 1985. The nature and properties <strong>of</strong> soils. 9 th Edition. Macmillan Publishing Co., 866 3 rd Ave., New York, New York, U.S.A. pp14-16.<br />

73<br />

when is this exercise most<br />

appropriate?<br />

ɶ In FFS, TOT, and<br />

VST sessions, as<br />

component <strong>of</strong> topic on<br />

‘Soil Conservation and<br />

Management’ or ‘Soil<br />

Biodiversity’; and<br />

ɶ When farmers want to<br />

learn more improved soil<br />

management practices<br />

from other farmers that<br />

will increase waterholding<br />

capacity <strong>of</strong> their<br />

soils.

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