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Last modified
11/23/2009 10:51:20 AM
Creation date
10/4/2006 9:32:59 PM
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Floodplain Documents
County
Statewide
Title
Determination of Channel Change for Selected Streams, Maricopa County, Arizona
Date
1/1/2002
Prepared For
Maricopa County Arizona
Prepared By
USGS
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br /> 6,000 <br />Cross-sectional area I- <br /> 5,000 w <br /> w <br /> u. <br />. . w <br />. a: <br /> " <br /> 4.000 ::;) <br /> 0 <br /> VJ <br /> :1; <br /> <i. <br /> Daily mean w <br /> 3,000 a: <br /> discharge " <br /> ...J <br />. " <br /> z <br /> 0 <br /> 2,000 >= <br /> '-' <br /> w <br /> VJ <br /> en <br /> VJ <br /> 0 <br /> 1,000 a: <br /> '-' <br /> <br />site. Several current-meter measurements of dis- <br />charge were made from the bridge, and these <br />measurements provide information about scour <br />and fill during high flows. <br /> <br />Gila River at Estrella Parkway, near <br />Goodyear, has a drainage area of 45,585 mi2. Only <br />large regional storms cause the river to flow <br />naturally because the river and most of its large <br />tributaries are regulated by dams. Sediment size in <br />the channel ranges from sand to cobbles. The <br />overbank area is an assortment of sand and gravel <br />deposits. Prolonged low flows are common at this <br />site because of wastewater-effluent discharge <br />upstream. <br /> <br />Bridge-measuring section.- Five current- <br />meter measurements of discharge were made <br />between January 6 and February 5, 1993. The <br />measurements ranged from 12,500 to 122,000 ft3/s <br />and were made during floodflow that reached a <br />peak discharge of 162,000 ft3/s at the gaging <br />station on January 9. Daily mean discharge and <br />cross-sectional area at the gaging station during <br />this period are shown in figure 9. <br /> <br /> 140.000 <br />0 <br />z <br />0 <br />'-' 120.000 <br />w <br />VJ <br />a: <br />w <br />0- <br />I- 100,000 <br />w <br />w <br />u. <br />'-' <br />a; 80,000 <br />::;) <br />'-' <br />:1; <br />ui <br />(!l 60,000 <br />a: <br />" <br />J: <br />'-' <br />~ 40.000 <br />0 <br />z <br />" <br />w <br />:2 <br />>- 20,000 <br />...J <br /><( <br />0 <br /> 0 <br /> <br /> <br />Using the cross section of January 6, 1993, as <br />a basis of comparison, the cross section measured <br />on January 9 shows several feet of scour mostly in <br />the deepest part of the channel (fig. 10). The cross- <br />sectional area doubled in relation to the reference <br />elevation of 12 ft (figs. 9 and 10). The measure- <br />ment made after the peak shows a 12-percent de- <br />crease in cross-sectional area. Subsequent cross <br />sections that were measured at lower discharges <br />show little additional change. <br /> <br />Hassayampa River <br /> <br />The Hassayampa River drains an area of about <br />1,500 mi2 from near Prescott in the north through <br />Wickenburg and south to the Gila River near <br />Goodyear (fig. I). Downstream from the gaging <br />station, Hassayampa River near Morristown, the <br />river becomes entrenched in the alluvium of the <br />Hassayampa Plain, a large alluvial basin between <br />the White Tank Mountains on the east and the low- <br />er Belmont Mountains on the west. The upper <br />reaches of the Hassayampa River are characterized <br />by steep, high-energy channels that have gravel <br /> <br /> <br /> <br />11 16 21 <br />JANUARY 1993 <br /> <br />6 <br /> <br /> <br />26 <br /> <br />31 5 9 <br />FEBRUARY 1993 <br /> <br />o <br /> <br />Figure 9. Daily mean discharge and cross-sectional area, Gila River at Estrella Parkway, near Goodyear, <br />Arizona, 1993. <br /> <br />14 Determination of Channel Change for Selected Streams, Maricopa County, Arizona <br />
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