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<br />003\)83 <br /> <br />78 <br /> <br />CONGRESO GEOL6GICO INTERNACIONAL <br /> <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, <br /> <br />"". ". <br />".J'i'> <br />c';".": , <br /> <br />,",ii,', <br />X')?J <br /> <br />. ~~' <br />"L;(}.:::i:\:: <br /> <br />",">",)"', <br />ie,.',;;:, <br />,..... 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