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by: Laplante, Albert A. -- Division of Agriculture and Home Economics
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NOTE: Due to difficulty in scanning the original, this page was retranscribed on 29 March 2013 by MARC Digital Publications Staff. All efforts were made to preserve the integrity of the original (including spacing of the document).
¹ Professor of Agriculture and Chairman of the division of Agriculture and Home Economics at the College of Guam. Laplante, Albert A. The Soil Units of Guam and their Agricultural Capability Oct 1964 Div. of Agriculture and Home Economics, College of Guam Bulletin 2
00003
The Soil units of Guam and their agricultural capability By
Dr. Albert A. Laplante¹
Introduction
“The soil may be defined as a natural body, built in profile form from a variable mixture of
broken and weathered minerals and decaying organic matter, which covers the earth in a thin layer and
which supplies, when containing proper amount of air and water, mechanical support and, in part, food
for plants.”
The management of this mass of minerals, organic matter, water and air is, therefore, the key to
agricultural development.
Soil Components
A silt loam surface soil in the best condition for plant growth contains:
45 percent mineral matter
5 percent organic matter
25 percent air
25 percent water
Importance of Air and Water
Without the proper proportion of air and water in soil, plant roots cannot find: (1) space to
grow, (2) mineral nutrients, since all mineral nutrients must be dissolved in water before entering the
plant and (3) the oxygen which is essential for growth and development.