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<br />78
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<br />CONGRESO GEOL6GICO INTERNACIONAL
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<br />derived from the Greck and means Hdry plant." Cacti are excellent examples
<br />of xerophytes,
<br />Phreatophytes are plants that habitnally obtain their water supply from the
<br />water table either directly or thorugh the capillary fringe (Meinzer, 1923, p,
<br />55). The term phreatophyte also is derived from the Greek and means "well
<br />plant." The form is apt, for by sending their roots to the water table they actual-
<br />ly dig their own wells and are able to pump their own supply of water, The
<br />distinction between xerophytes and phreatophytes with respect to their sources
<br />of supply is shown in Figure 1. It is important that this distinction be kept in
<br />mind when considering the hydrology of arid regions. Although the area oc.
<br />cupied by xerophytes is much larger than the area occupied by phreatophytes,
<br />the latter have a greater effect than the former on the water that is available
<br />for man's use.
<br />The relative importance of the roles that these two classes of plants play in
<br />the hydrology of arid regions is shown by considering their position in the
<br />hydrologic cycle. Figure 2 depicts graphically a simple hydrologic cycle-that
<br />for an undeveloped closed basin in an arid region, In this endless cyele of
<br />water movement through the atmosphere to the land, and back to the atmosphere
<br />again, the wa.ter moves as liquid and as vapor through a maze of overland and
<br />undeground routes. The diagram shows: (I) the distinction between the sources
<br />01 supply for these twoelasses of plants-soil water for xerophytes aud ground
<br />water for phreatophytes; (2) the relative positions of the supply reservoirs;
<br />and (3) the paths of the movement of water to and from them,
<br />Consider first the soil-water reservoir, which is replenished largely by the
<br />seanty precipitation and to a lesser extent by occasional overland runoff. The
<br />water in this reservoir is not directly available to man, for he cannot extract
<br />it in liquid form. It may be available to kim indirectly in the products of plant
<br />growth, but in this form it does not quench his thirst or meet his other every-
<br />day needs. Water that eute'IS the soil in quantities that are in excess of its mois-
<br />ture-holding capacity eventually becames available to man through dawnward
<br />percolation as recharge to the ground-water reservoir. Generally in arid regions
<br />the excess i's quite small, owing in part to the sca.ntiness of the precipitation and
<br />in part, as shown by the diagram, to depletion of the soil-water reservoir by
<br />the transpiration of xerophytes.
<br />In contrast, the water in the ground-water reservoir is avaliable to man.
<br />The reservoir is recharged by the percolation of excess soil water and by seepage
<br />from streams and lakes. The water is available ..0 man either directly through
<br />spring discharge and seepage to streams and lakes or indirectly through wells,
<br />tunnels, or ditches. In some localities it is the only supply of water. This water
<br />is available to phreatophytes also, which, through their draft on ground water,
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