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Last modified
7/14/2009 5:02:33 PM
Creation date
5/22/2009 4:49:07 PM
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Template:
UCREFRP
UCREFRP Catalog Number
8142
Author
Horn, M. J.
Title
Nutritional Limitation of Recruitment in the Razorback Sucker (
USFW Year
1996.
Copyright Material
NO
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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />~ <br />;>;: <br /> <br />f <br />i~ <br /> <br />111' <br />'Ii <br /> <br />12 <br /> <br />national issue, and federal subsidies were used to construct a series of major dams (Table <br /> <br /> <br />2), the foremost of which was Hoover Dam, completed in 1935 to impound Lake Mead. <br /> <br />I;, <br /> <br />~ <br /> <br />~, <br /> <br />High dams on the lower Colorado River controlled flooding, so channelization, <br /> <br />levee construction, and other amenities to manipulate and deliver water proceeded apace <br /> <br />with increasing demands. The dams also produced electricity for pumps and other <br /> <br /> <br />devices to expand agriculture and develop industry. Domestic water supplies were <br /> <br /> <br />abundant, and along with expanded economy and a salubrious "Sunbelt" climate, <br /> <br /> <br />stimulated retirement and recreation industries, such that human populations burgeoned <br /> <br /> <br />and their demands on resources increased. <br /> <br /> <br />Reservoirs retain sediment, effectively ending bedload transport of inorganic <br /> <br /> <br />material from upstream and curtailed transport in the form of suspended turbidity. <br /> <br /> <br />Chemical nutrients are retained due to biologic uptake and sedimentation under lentic <br /> <br /> <br />conditions, although release of hypolimnetic water may mitigate that effect (Stanford <br /> <br /> <br />1994). Organic materials from the watershed are similarly affected. Particulate sediment <br /> <br /> <br />and dissolved organics are altered and often reduced under reservoir conditions. <br /> <br /> <br />Downstream impacts include significant changes in thermal regimes and increased <br /> <br /> <br />degradation of bottom and banks by clear water with high erosional competence, the latter <br /> <br />compensated for by further channel modification (Williams and Wolman 1984). The <br /> <br /> <br />process of degradation selectively removes fine sediments, leaving large-particle or <br /> <br />"armored" bottoms. Additionally, discharge patterns downstream from regulatory <br /> <br />-- <br />
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