EIS-0113_Section_9 - Hanford Site
EIS-0113_Section_9 - Hanford Site
EIS-0113_Section_9 - Hanford Site
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ss.<br />
M<br />
0044<br />
J.<br />
RECEIVED DQE-RL<br />
JUL 14 10<br />
WM DIVISION<br />
.2!Vcti MERL<br />
auL 1 4 1386<br />
WM DIVISION<br />
3d Thechances i i distribution of onosmanants sho po I/<br />
CF at the contami next. be migrated. 2/ that contamination has<br />
passed a w<br />
heren<br />
ontamnation a I. f ound iil<br />
n the soil<br />
(betwe ,,the p ]t t d if t . and3/that<br />
3.5.2.44 ont amenatio mov have extended to the ground water an. been<br />
vetl before retortion. It is . also paible ss that, i/ the<br />
,'char act erizatlon" data has c sid...his 3<br />
In either r<br />
ontamination s not abe proven to be<br />
contained by the "in place" design of Figure n9.<br />
35.6 . .<br />
3e Climate stability prdvidino continuation of present<br />
rid conditions,.r essential requirements for the Proposed<br />
-place" design (with no events oreater than double present<br />
rage r i.4.11). On a Iong term basis this is not likely nor<br />
er ifiable. Past climatic fluctuations a shown by palynological<br />
and marine st,.ti,r.phir data indicate major fluctuations Io the<br />
past (Holocene time).<br />
3c Risk tc. the water s`up ply of Cre non s m ,ibisw<br />
ater table.. at Boardman and potential for nf'lt t' nfr om the<br />
ncludino Portland has not been oval noted. The extremely low<br />
Columbia Raver M1as not been add ... b.d. In the event of Bull Run<br />
water prcblems Portlantlhas the option of using the newly<br />
developed Portland welt field a a back upsupply, yet the<br />
drawdown of aquifers in Portland Could result in depressed water.<br />
tables like those at Boardman. .Infiltration of Columbia River.<br />
water into the Portland well field aquifers is real possibility<br />
under that easily passible .condition.<br />
3.5.2.44<br />
y'l<br />
W<br />
Environmental Values and Coate are net differentiated<br />
The eaJor. problems with the MIS are the failure to<br />
.cognize the ..Jor anvironmemtal values, and the uncontested and<br />
2.3.1.2 untes ad easumption of continuation of the amistinq precedent for<br />
nuclear processing and disposal use of the <strong>Hanford</strong> site without<br />
site suitability comparative analyeb.<br />
3 .2.6.2<br />
p<br />
3. "Value" and " oat" are not differentiated nor<br />
valuated. Water has value but<br />
me cost<br />
(only the cast of<br />
delivery). The value of the Columbia River and the adjacent<br />
sedimentary basins to the livelihood of the region are very o eat<br />
but are not atltlressed. The value and cost of less of purity , of<br />
the Columbia River is not addressed.<br />
In this B<strong>EIS</strong>, cost is calculated in the short term as<br />
3.2.6. 8<br />
dollar. and risk to live% in the disposal process.<br />
No comparison is made of the potential long term<br />
productivity of the water and ..it of the .,.a, for a ample, a<br />
an agricultural site (and the number of lives which could be<br />
supported in the area) compared to the long term productivity and<br />
r}sk ds a hazardous and nuclear waste site.<br />
31, Comparison of the long term cultural value of the<br />
special soil and drainage conditions in the Pasco Basin Manford)<br />
to the areas less suitable for agriculture is not evaluated.<br />
3.2.6.2<br />
Eco nomicgeographyanalysee r<br />
should provide greater recognition of<br />
the comparison to other geological sites most probably much<br />
better suited for waste disposal and much less suitable for<br />
agriculture and productive land use.