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<br />'l <br />,r~ <br />. , <br /> <br />STEADY, UNIFORM-FLOW <br />ASSUMPTIONS <br /> <br />Width, depth, and flow directio <br />little throughout reach 'jilfJ" <br />Water-surface profile and energy graorel1t <br />are parallel to the streambed ,< <br /> <br />\y;.~"" <br /> <br /> <br />Although it rarely exists in natural stream.s, <br />uniform flow can be assumed if the changes <br />are small. <br /> <br /> <br />