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TheImprovement ofTropical and Subtropical Rangelands

TheImprovement ofTropical and Subtropical Rangelands

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CRITERIA FOR PLANT SELECTION 193<br />

ADAPTATION TO sons<br />

Soil suitability for plant production may be based upon a combination<br />

of water budget <strong>and</strong> nutrient status (including oxygen).<br />

These, in turn, depend upon physical <strong>and</strong> chemical characteristics.<br />

The main physical characteristics to consider are discussed below.<br />

Tut••<br />

Texture, particularly of the topsoil, largely controls permeability<br />

<strong>and</strong> water intake, <strong>and</strong> therefore water budget. Texture also controls,<br />

to some degree, nutrient status. Some species are adapted to coarsetextured<br />

soils (psammophytes), others are suited to fine-textured<br />

soils (pelophytes), <strong>and</strong> still others may be little affected by the texture<br />

factor. Textural differences play a large part in the ability of seeds<br />

to emerge or roots to penetrate dense soils composed of a majority of<br />

clay-sized particles that tend to form dense surface crusts when dry.<br />

structure<br />

Structure affects soil permeability <strong>and</strong> drainage, redox potential<br />

(<strong>and</strong> therefore waterlogging), <strong>and</strong> temporary or permanent aerobic or<br />

anaerobic conditions (root asphyxia, H 2 S toxicity, etc.). Some species<br />

can tolerate anaerobic conditions, while others are very sensitive <strong>and</strong><br />

fail to grow or survive.<br />

Depth<br />

Soil depth, in conjunction with permeability, controls water storage<br />

capacity, which is a key characteristic in arid <strong>and</strong> semiarid l<strong>and</strong>s.<br />

Deep soils may store large amounts of water during short rainy periods<br />

where it is subsequently available to deep-rooted plants, thus<br />

buffering the effect of climatic aridity. In the arid zone, high productivity<br />

is achieved on deep s<strong>and</strong>y soils because virtually all rain is<br />

stored <strong>and</strong> then released to plants. Under higher <strong>and</strong> more regular<br />

rainfall, however, deep s<strong>and</strong>y soils tend to be relatively less productive<br />

because oflower nutrient status. Nutrients, as well as water, can<br />

be a limiting factor to plant growth.<br />

Shallow, stony, impervious soils, on the other h<strong>and</strong>, hold little<br />

water <strong>and</strong> can cause water stress in plants. Shallowness <strong>and</strong> imperviousness<br />

may, however, be corrected with adequate treatment, such as<br />

ripping, in order to break an impervious caliche (indurated calcium

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