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TheImprovement ofTropical and Subtropical Rangelands

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194 IMPROVEMENT OF TROPIOAL AND SUBTROPIOAL RANGELANDS<br />

or magnesium carbonate) hardpan. Pitting, chiaeling, <strong>and</strong> sweeping<br />

may considerably increase water intake by breaking a superficial<br />

thin-clay-sealed or loam-sealed pan that may have rendered the soil<br />

almost impervious.<br />

The sealing of an arid-lone soil surface is a very potent factor<br />

in desertification <strong>and</strong> is sometimes reinforced by lichens or by<br />

microscopic blue-green algal encrustations. This sealing can be overcome<br />

by breaking the soil surface <strong>and</strong> roughening it with mechanical<br />

tools or by the hoof action of grazing animals, a technique that may<br />

greatly increase productivity. Conversely, if heavy traffic by hooves<br />

or equipment occurs when the soil is wet, compaction may occur to<br />

exacerbate the existing low permeability.<br />

Water Storage Capacity<br />

The role of water storage capacity obviously increases with aridity<br />

<strong>and</strong> rainfall variability. All the ancient techniques of "runoff<br />

farming" over S,OOO years old in the Near East, are based on water<br />

storage capacity-eollecting surface runoff <strong>and</strong> storing it in the soil<br />

profile of run-in areas (Evenari et al., 1971).<br />

Storage capacity may be increased by using well-known techniques<br />

tending either to reduce runoff (pitting, contour furrowing, or<br />

contour benching) or to collect runoff water <strong>and</strong> use it on another<br />

nearby site employing water harvesting <strong>and</strong> spreading techniques.<br />

These techniques, which may be 2,OOO-S,OOO years old, make<br />

it p088ible to grow crops on arid-zone soils. Under the me8k4t or<br />

je880ur system techniques in the arid zone of Tunisia <strong>and</strong> Libya, for<br />

example, over 10 million productive olive trees have been grown for<br />

centuries in areas receiving from 80 to SOO mm of precipitation (Le<br />

Houerou, 1959).<br />

Chemical Characteristics<br />

Among soil chemical properties, pH is one ofthe most important.<br />

Some plant species require acidic soil (acidophilic), others require alkaline<br />

conditions (basophilic), <strong>and</strong> a few are relatively indifferent to<br />

this factor. Nutrient status may also be a serious limiting factor. In<br />

many instances, however, nitrogen, phosphorus, or sulfur deficiencies<br />

can be overcome either by using fertililers, ashes, or manure, or<br />

by using plant species that have low nutrient dem<strong>and</strong>s. The presence<br />

of toxic elements should also be taken into consideration. The

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