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<br /> <br />EPHEMERAL STREAMS <br /> <br />11 <br /> <br />Figure 9 presents the data for suspended load at <br />various discharges (the suspended-sediment rating <br />curve) measured at two Geological Survey sediment <br />stations. The same section is used for both discharge <br />and suspended-load measurements at the Domingo <br />station on the Rio Galisteo. For the other example, the <br />sediment station is located 11 miles downstream from <br />the gage on the Rio Puerco at Cabezon. Because no <br />major tributaries enter in this reach of the stream, the <br />sediment and discharge records may be considered <br />essentially comparable. <br />The data from sediment measurements in small <br />ephemeral streams are shown on figure 10, along with <br />curves for the two sediment stations. In each arroyo <br />cross section we measured only a single flood, \vhereas <br />in regular sediment operations each measurement <br /> <br />represents generally a different hydrograph rise or <br />different day. Nevertheless, lines drawn through our <br />meager data agree very well with the sediment-rating <br />curves of the regular sediment stations. Furthermore, <br />the scatter of our data obtained by wading measure- <br />ments (fig. 10) is no greater than that for the stations <br />(fig. 9). This suggests that the suspended-load rating <br />curve at a given cross section in a western ephemeral <br />stream can be approximated by a series of measure- <br />ments during one or two floods. <br />The relation of suspended load to discharge has bee" <br />expressed as <br /> <br />L=pQ' <br /> <br />where L is suspended load in tons per day (Leopold and <br />.\1addock, 19.53). Values of j (slope of the suspended- <br />sediment rating curve) for arroyos range from 1.09 to <br /> <br /> <br /> <br /> <br />Rio Galisteo at Domingo. New Mexico <br /> <br />100,000 <br /> <br />. <br />. <br />. <br /> <br />>- <br /><< <br />o <br />~ <br />w <br />~ <br />on <br />z <br />o 10,000 <br />" <br />;; <br />ci <br /><< <br />g <br />" <br />z <br />w <br />" <br />o <br />w <br />on <br />, <br />o <br />w <br />o <br />z <br />w <br />~ <br />on <br />=> <br />on <br /> <br />. <br />. <br /> <br />,. :- <br /> <br />1000 <br /> <br /> <br />. <br /> <br />. <br /> <br />. <br />I . <br />100 ~-. <br />.'+:. <br />~. <br />,-. <br /> <br />1 <br />.- <br />I <br />. <br /> <br />10 <br /> <br /> <br />10 <br /> <br />100 <br /> <br />DISCHARGE, IN CUBIC FEET PER SECOND <br /> <br />10 <br /> <br />100 <br /> <br />1000 <br /> <br />{' <br />.... <br />9.4.-1. <br />i??L <br />.0 <br />" <br /> <br />. <br /> <br />500 <br /> <br />Rio Puerco at Cabezon, New Mexico <br /> <br />'I' <br />..... <br />.'" <br />o <br />'" <br /> <br />1000 <br /> <br /> <br />,. <br />. <br /> <br /> <br />I <br />. <br /> <br /> <br />FIGl'RK 9.-Suspended.sediment rating curves for Rio Galisteo at Domingo, N. MH., and for Rio Puerco near Cabezon, N. Mex., measured one-fourth mile above the <br />mouth of Chico Arroyo. <br />