ML20006F951

From kanterella
Jump to navigation Jump to search
Trip Rept of 900205 Visit to Albuquerque,Nm Re Review of Geological Data Collected by DOE at Ambrosia Lake Site.Tres Hermanos Unit C Should Be Labeled as Poorly Sorted Sandy Mudstone,Not Sandstone
ML20006F951
Person / Time
Issue date: 02/09/1990
From: Grimm J
NRC OFFICE OF INSPECTION & ENFORCEMENT (IE REGION IV)
To: Randy Hall
NRC OFFICE OF INSPECTION & ENFORCEMENT (IE REGION IV)
References
REF-WM-67 NUDOCS 9003010387
Download: ML20006F951 (3)


Text

3

,3 t

')

'b pq sit 04 _

UNITED STATES -

As

/

NUCLEAR REGULATORY COMMISSION s

',r

[

r f

i REGION IV i

,e URANIUM RECOVERY FIELD OFFICE

' 6 f;

' em, D OX 25325 DENVER, COLORADO 80225 FEB 91990

t' URFO:JPG Docket No. WM-67 a

3

. MEMORANDUM FOR:

Ramon E. Hall Director FROM:

Joel P. Grimm Project Manager

^

SUBJECT:

DATA REVIEW: DOE'S AMBROSIA LAKE UMTRA PROJECT SITE f

Introduction

,j

! k On February 5,:1990, I traveled to Albuquerque, New Mexico, to conduct a review of geological data collected by the Department of Energy (DOE) at the Ambrosia p

-Lake,-New Mexico, UMTRA Project site.

My purpose was to observe geological samples ~ collected from wells drilled at the site..- The samples consist of drill

"(cuttings and rock core recovered from holes drilled for site characterization and installation of monitor wells..The first goal of the data review was to familiarize myself with the general geological description of rock types which underlie the site.. The second goal was to resolve specific discrepancies

. between 1ogsxof various wells, verify DOE's interpretations of geological

~

l' conditions, and collect information missing in DOE submittals.

t

Background

The Ambrosia Lake tailings pile overlies alluvial valley fill and the lower.

stratigraphic section of the Mancos Shale.

The lower Mancos in this area 4

consists of typical, dark grey, dense claystone, interbedded with three

~~

coarser grained units, known in ascending order as the Tres Hermanos A, B, and.

C sandstones.

The site is then underlain by the Dakota Sandstone and Morrison b>

Formation, which are of less significance to the remedial action.

e Results

Rock core is stored in a laboratory / warehouse operated by DOE's Technical Assistance Contractor (TAC).

Core sampled from most of the bedrock section was available from wells numbered 683 and 684.

Core from selected intervals was collected for wells numbered 773, 779, and 781.

'The most important result of the data review was my observation that the Tres Hermanos members are not coarse grained, yellow grey, porous sandstones so

[$

900301038'7 900209 PDR WASTE

(

.WM-6'7_

PDC p

i

FEB 91990 2

typical of other_ Cretaceous sandstones in western New Mexico.

Rather, the Tres Hermanos,. most notably unit C, is very dark grey, fine grained sandstone and siltstone, with a high percentage of shaley or clayey matrix material.

The rock appears very poorly sorted and displays a large degree of uneven and contorted bedding.

Samples recovered from the interval interpreted as the Tres Hermanos B include a light grey, fine-to medium grained sandstone.

All samples taken from intervening sections consist of dense, dark grey, fossiliferous claystone typical of the main body of the Mancos Shale.

Discussion Tres Hermanos unit C should probably not be labled a sandstone, but rather a poorly sorted sandy mudstone.

My observation probably supports DOE's interpretation that the Tres Hemanos C provides only low quantities of poor quality ground water.

DOE's Remedial Action Plan (RAP) probably could be revised to more accurately. indicate the lithology of the Tres Hermanos-sandstones.

This revision would more accurately reflect stratigraphic conditions at the site, and could contribute to a more technically sound and complete ground-water protection strategy.

Summary The primary goal of the data review was achieved because information was collected which is not-only difficult to portray in text, but also difficult to observe in the field.

The observations made will provide significant input to the staff's Technical Evaluation Report (TER), both on the geologic and ground-water protection sections.

The second goal will be satisfied with submittal by DOE / TAC of the following information:

1)

Lithologic logs of series-600 wells, drilled early in 1989, but omitted from the most recent version of the RAP.

This information was provided for my retention during the data review.

2)

Lithologic logs of series-700 wells, drilled in 1985, which have been recently revised, and supposedly are more accurate than a version of drilling logs submitted in DOE's 1987 "Information for Bidders."

Submittal of these data is in preparation.

)

The data review was arranged by DOE's Project Managers Michael Abrams and Steven Hamp.

I was assisted by Mr. Gerald Linday, TAC.

Additional information is being prepared for submittal by Mr. Erik Storms, TAC.

oel P. Grimm Project Manager

8 c-l.l; W u.

.t u

,w

..~

[

WM-67/jpg/90/02/05/M

~

DISTRIBUTION.

Docket File WM-67 fPDR/DCS g'!.

URF0 r/f.

.d{'-

AB8each, RIV.~-

LLO Branch, LLWM

._ y -

M JGrim -

in

=

l

'l i..,

CONCURRENCE:

DATE:

!)

1/Skd JGrim/URF0/1v

(;;.

EHawkins/URF0 7 70 -

REHall/URF0.

78 e

j[s;.

$l ~.

5

.j --

dj t

k '

4:

.