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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.

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