000	02094cam  2200313za 4500
001	9.861449
003	CaOODSP
005	20221107160747
007	cr |||||||||||
008	180831s1967    onca||||o    f000 0 eng d
040	|aCaOODSP|beng
043	|an-cn-sn
086	1 |aEn36-515/10E-PDF
100	1 |aVan Everdingen, R. O.
245	10|aDiefenbaker Lake |h[electronic resource] : |beffects of bank erosion on storage capacity / |cR.O. Van Everdingen.
260	|aOttawa : |bDept. of Energy, Mines and Resources, Inland Waters Branch, |c[1967]
300	|aiii, 21 p. : |bill.
490	1 |aTechnical bulletin - Inland Waters Branch ; |vno. 10
500	|aDigitized edition from print [produced by Environment and Climate Change Canada].
504	|aIncludes bibliographical references.
520	|a"The creation of a surface-water reservoir exposes valley slopes, that were originally formed by glacial or runoff erosion, to the erosive energy of two or three new agents: waves, ice and, under the right circumstances, groundwater movement. This will result in accelerated erosion of the reservoir banks during the early years of the reservoir's useful life. Continued modification of shore profiles will adapt the exposed slopes to the new conditions and the erosion rate will consequently decrease with time. The effect of bank erosion in terms of reservoir economics will usually be threefold:(1) increase in the surface area of the reservoir, resulting in increased evaporation, (2) formation and increase in the width of an accumulation shelf (beach) and (3) decrease in storage capacity by deposition of erosion products"--Introd.
693	4|aBeach erosion
693	4|aReservoir sedimentation
710	1 |aCanada. |bEnvironment Canada.
710	1 |aCanada. |bInland Waters Branch.
710	1 |aCanada. |bDepartment of Energy, Mines and Resources.
830	#0|aTechnical bulletin (Canada. Inland Waters Branch)|vno. 10|w(CaOODSP)9.861115
856	40|qPDF|s1.25 MB|uhttps://publications.gc.ca/collections/collection_2018/eccc/En36-515-10-eng.pdf