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1 <br /> vslue problem creating this phenomenon It Co is spreading process Hence, considering lateral <br /> the masured concentration at the waste boundary ing to be insignificant, we are lett with <br /> and CL is rhe concentration of the ground water <br /> further downgradient at any point L (the alternative CO = 1 + 2L (DT/V, L)"1 <br /> boundary), then CL L, <br /> CL ' 1 _ 1 The interesting question regarding Verrical <br /> Co I + 2(L/L,)(DT/VcL)'" 1 + 2 [(DT 0"/L,] /Spreading is as tollows At what distance L' trod <br /> the solid waste boundary will the maximum <br /> _ (2) takejlace due to transverse spreading in a 4crt-r� <br /> where L is the distance to the alternative boundary, planes This will obviously occur where the cori;z=,- <br /> and L, is the horizontal width of the contaminant inant plume occupies most of the thickness of Uc <br /> ' stream at the waste boundary (Figure 1(a)] aquifer BearS1979, p 252) estimates this distarc: <br /> A more realistic assessment may be obtained to be about 10 to 15 times the aquifer thickness <br /> by-1 t7wo-dimensional front where there is transverse ItLthc general case of vertical spreading [Figure <br /> ' dispersion in two directions perpendicular to the 1(b)] , we expect the spreading thickness to be <br /> flow lines Hence, the front will not only spread approximated by L2 + (DT L/Vc)'" where L, <br /> laterally but vertically as well [Figures 1(a) and corresponds to the thickness-of the plume at <br /> ' 1(b)] If the transverse dispersion coefficient is the the waste boundary, andf`L`is any given distance <br /> same in both directions, the conservation of mass from the boundary As in all previous cases, the <br /> principle implies diffusio0_1 c <br /> .Dgti'(DT L/Vc)'5 is taken as an approxi- <br /> mate measure for the spread For the condition <br /> CO = [I + 2 (DTO [1 + - (DT t) ] (3) that L corresponds to the distance from the waste <br /> t � <br /> CL L, L, facility where the contaminant plume occupies <br /> ' or most of the aquifer thickness [L', Figure 1(c)] , the <br /> available spreading thickness equals the aquifer <br /> 2L 2L thickness"i�so that <br /> Co. _ [I + --' {DTNc!-)� � [1 + -- (D-r/Vc L)11] {4) <br /> CL L, L, H = L2 + (DT L'/bc)", (6) <br /> where the dimensions of the contaminant at the This gives <br /> l source are L,(horizontal) and(L2`(vcrtica.l), the - <br /> 1 latter being obtained from inventory wells a;_the' L' _ Vc (H — L )2 (7) <br /> waste boundary p 2 <br /> T <br /> As L, will in general be much larger than L2, The distance L',can be regarded as a "t-fixing leng h" <br /> the second bracketed quantity on the right-hand <br /> side of equation (4) will generally dominate the wherein the contaminant plume obtains maximum <br /> dilution due to vertical spreading From the conser- <br /> vation of mass statement <br /> Ct- <br /> where(C�ts the concentration at L' <br /> L, L Consider the following eYampie For Vc/DT <br /> so�, r- equals one (meter)", L, equals 2 meters, and an i <br /> sal tai aquifer thickness H of about 10 meters, L' is calcu- <br /> L' lated to be about 64 meters,and CL', equals 0 2 Co <br /> t 1 1 i f Hence, the limit to vertical spreading in this case 1 <br /> _ __ Wv4.Tchy_ _ _ _ __ _ occurs about 64 meters rrom the waste facilityL: <br /> H Transverse spreading throughout this distance will <br /> result in a lowering of the concentration to about <br /> 20 percent of the value observed at the waste <br /> Fig 1 Geometrical s reaaing of contaminant plume in a boundary ,fin increase in veloc.ty relative to trans- <br /> la) horizontal plane, b) vertical plane,and (c) vertical verse dispersion increases the distance L' but has no I <br /> Plane where the cont mant occupies the full aquifer effect on the dilution potential as erpiessed by <br /> thickness equation (8) An increase in aquifer thickness H, <br /> 306 - <br />