Below are the first 10 and last 10 pages of uncorrected machine-read text (when available) of this chapter, followed by the top 30 algorithmically extracted key phrases from the chapter as a whole.
Intended to provide our own search engines and external engines with highly rich, chapter-representative searchable text on the opening pages of each chapter.
Because it is UNCORRECTED material, please consider the following text as a useful but insufficient proxy for the authoritative book pages.
Do not use for reproduction, copying, pasting, or reading; exclusively for search engines.
OCR for page 375
780,000
770,000
o
760,000
750,QOO
1
e
Potantiai
ne~S~
Boundary
1
560,000
EASTING, M
570,000
1~01~n am,
In m~aar
[a: :: ~s~:i~I Tea Canyon TuM 0 22
modorataly welded
Tea Canyon Tu#
welded
Paintbrush Group
nonwe~ed 1u#
0.02
13.40
Topopah SpMng Tu#
fled 0.08
Rainier Mesa Tu# 0.06
PLATE 1 Spah~Hy dis~ibu[ed icon in bedrock Unix. From Flint and Flint (1994,
Figure 4 Id Tale 3~. Copyright 1994 by me Amedc~ Nuclei Society, Lo Crange Pay,
. .
Illmols.
OCR for page 376
UTM EASTING, IN METERS
545.000 550.000 555.000
o
o
o
CO
o
CD
A
I
a: 0
o $
LO
0
o
o
o
o
o
EXPLANATION
.,: - , JO
,
· 4
I:
1 0 20 30 40 50 60 70 80
NET INFILTRATION, IN MILLIMETERS PER YEAR
PLATE 2 Spatial distribution of net infiltration. From Flint et al. (1996a, Figure 39~.
OCR for page 377
-
\ ~ ui
\ ~ - I*73
\
\
.~
PLATE 3 NMRI flow profiles in fractures showing 2D slices through a 3D image of the
principal (A velocity component of water flowing inside the rock fracture. Fracture sam-
ple dimensions are ~36 mm by ~18 mm. (a) Two yz-slices with x = 4.7 and 15.2 mm, and
an xz-slice with y = 4.0 mm, parallel to the principal flow direction (indicated by the
round arrow); and three xy-slices with z = 2.8, 12.7, and 22.5 mm, perpendicular to the
principal flow direction; (b) two yz-slices with x = 4.7 and 17.3 mm, parallel to the
principal flow direction; (c) an xz-slice with y = 4.0 mm, parallel to the principal flow
direction; (d) three xy-slices with z = 2.8, 12.7, and 21.1 mm, perpendicular to the princi-
pal flow direction. Darker shades represent regions of higher velocity. The vertical scale
is highly exaggerated, since the image scale is in units of measured volume elements.
Control tubes are clearly visible on the two sides of the fracture sample. After Dijk et al.
(19991.
OCR for page 378
lo
lo
of
a)
en lo
1 ' C\l
cn '
. - lo
lo
lo
cM
lo
lo
cM
lo
lo
[e use Bun] ~
Depth (cm)
0 0 0 0 0 0
~ ~ ~ ~ O
0.05
1 I 1 I I
~..,,~ ~
:
...
l l l l
o
o
0.05
o ~
~ o
· .
o o
o o
CM
Depth (cm)
O O O O
~ ~ ~ O
I 1 i i , ~
,,~
. r . I , .~
O..
Ct
0
p~
~o (~) 0°
a~ c~ ~
~ ~ ·s
_ · C~
° ~o
CQ
0 4.°
Ct ~
0
~ 3
· - ~
~o
C~
s~ s~
~o ~ ~
a~ t0
~o ~ ~
5 ~
·= ~ o o
.=
~.s ~ o
. _1 ~ Ct ~
^ o ·~
. ~ oN
5_,
,= .
~ ~ ¢ ~
cd ~ o
o ~ ~ ~
P_ c~ ~ a~
.=
~ ~ o ~
o~ o ·
c~ ~ cn a~
Q ~ ~ ~
~ ^ o O
O ~ 1_
- ^
h.= ~
~o
OCR for page 379
O ~ ~ I ~
~ ~ ~ O ()
Cal
~ .
in
o
.
o
a)
o
la
to
in
o
Cal
o
Cal
C)
r
o
3
so
At
· ~
Cal
a;
o
3
o
NIL
.m
¢
[a
¢
OCR for page 380
~ 2.36E5
En
Lo
A
in:
o
~ 2.34E5
>
SD-
. . ~,
Model boundary
1.68E5 1.70E5 1.72E5 1.74E5
EAST N EVADA COORDINATES (m)
PLATE 6 A plan view of the three-dimensional UZ site-scale model domain, showing
grid and locations of boreholes (including perched water boreholes) used for model cali-
bration.
OCR for page 381
I
/
1 470
\
meters
(masl)
770 ~ 1~_
~~q.
1 68000
1 69000
100% Liquid Saturation Isosurface
Top surface of the Tac
(2x vertical exaggeration)
17000~~ L___ _ ~
E6Sting(~) 171000 ~ ~
1 72000
1 73000
239020
238000
236000
~23400(
231040
PLATE 7 Three-dimensional perched-water bodies near the base of the TSw, using the
permeability barrier conceptual model.
c
OCR for page 382
239000
238000
237000
236000
a)
Is
235000
a
a
234000
>
I 233000
a
z 232000
231000
230000
1 1 1 1 1 - 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1
mm/year
10
9
8
7
6
5
4
3
2
1
o
168000 170000 172000 174000
East Nevada Coordinates (m)
PLATE 8 Percolation flux (mm/yr) contours at the water table.
Representative terms from entire chapter:
principal flow
