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4 <br />GLOSSARY OF TERMS <br />Aggradation. - The raising of the surface of streambeds, flood plains, and the <br />bottoms of other water bodies by the accretion or deposition of material <br />eroded and transported from other areas. <br />Bed material. - The sediment mixture of which the bed is composed. <br />Bed-material load. - That part of the total load of a stream which is composed <br />of particle sizes present in appreciable quantities in the shifting portion of <br />the streamed. <br />Degradation. - The lowering of the surface of streambeds, flood plains, and <br />the bottoms of other water bodies by the removal of material from the <br />boundary. <br />Effective discharge. - The modal sediment-transporting discharge computed from <br />a sediment rating curve and flow-duration data for a stream for a given time <br />period. <br />Quasi-equilibrium. - The condition where sediment supplied to a channel is <br />transported with the available discharge. No net accumulation or depletion of <br />sediment in the bed, banks, or flood plain occurs under this condition. <br />Regime equation. - A mathematical expression relating a channel dimension, <br />such as width, to a measure of streamflow, such as mean annual discharge. <br />Additional channel parameters such as bed-material size, channel slope, chan- <br />nel depth, and bed-material load have also been used in regime equations. <br />ii