I'r - Memorial University of Newfoundland

More documents

Recommendations

Info

Figure 5.1.1 1 Statioo locations and bathymetry afte r Ristic and Ristic (1985). Note the complicated bottom topography in the DOrtheastern pari <strong>of</strong>tbe Western Basin.
Page 3:
POLYCYCLIC AROMATIC HYDROCARBONS IN
Page 6 and 7:
composition. Portions ofthe lake th
Page 8 and 9:
TABLE OF CONTENTS . ABSTRAcr._._ _
Page 10:
6. CONCLUSIONS_._ _....._._._ _ ._
Page 13 and 14:
FIGURE 3.104 CONfIGURATION OF ISOCH
Page 15 and 16:
FIGURE 4 .2.12 SAMPLES AND PROMINEN
Page 17 and 18:
fIGURE 5.3.1 DESCR1Pl1VE MODEL OF S
Page 19 and 20:
APPENDIX B 3 _ T HEoerwt Of A PtUNC
Page 21 and 22:
Ip » Ideno(l,2.3 cd)pyrene NIST =
Page 23:
Figure L 1.1 The 16 parental polycy
Page 26 and 27:
After release by the primary source
Page 28:
decomposition processes (O'Malley e
Page 32:
Figure 2.1.1 The Great Lakes draina
Page 35 and 36:
;: Duluth Chicago 1 J Lake Superior
Page 38 and 39:
are the Black River, the Cuyaho ga
Page 41:
Figure 1.1.5 The pattern of permane
Page 45 and 46:
sedimentary basins, Western. Centra
Page 48:
Figure 2. 1.8 Summer (July) air and
Page 52:
Natural Resources: The lower Great
Page 57 and 58:
American waters under the current U
Page 60 and 61:
continuously overflowed com bined s
Page 63 and 64:
3.1 EXPERIMENTAL 3. METHODS 3.1.1 S
Page 66 and 67:
Table 3,1.1 Locations and types ofs
Page 68:
Figure 3.12 Extraction and purifica
Page 72 and 73:
hexane. 2) the unsaturated aliphati
Page 75:
this problem. Ratios ofthe two stab
Page 78:
Figure 3. 1.4 Configuration ofIsoch
Page 82 and 83:
3.2.1 UNl- AND BIVAJUATE METHODS Th
Page 84:
f igure 3.2. 1 Mean and range (± s
Page 87 and 88:
utilized the same instrument (Isoch
Page 90 and 91:
Selecting lIt1J'iahlu: It was demon
Page 92 and 93:
w- _ 71
Page 95 and 96:
seven variables with fewer missing
Page 97 and 98:
analysis also employed a greate r n
Page 99:
description. The second cluster ana
Page 104 and 105:
elationships between different site
Page 107:
Figure 4.1.3 Regression ofthree fir
Page 112:
Figure 4.[.5 Isotopic composition (
Page 116:
Figure 4.1.6 Weights ofvariables (c
Page 120:
Figure 4.1.8 Distri bution ofsample
Page 123 and 124:
those at the majority ofstations. S
Page 126 and 127:
Ion, 969, 971, 357, 358). In additi
Page 129:
Figure 4.2.3 Samples and prominent
Page 132 and 133:
analysis supported some ofthc previ
Page 135 and 136:
, ", Is , , >\ ryr " II ,- - , I ,
Page 137 and 138:
11'
Page 139:
sources (Fi g. 4.2 .5c). This compo
Page 143:
Figure 4.2.7 The relative contribut
Page 146 and 147:
".1.1.2 Miring CllrIIU (isotopic co
Page 149:
Figure 42.9 Samples and promin ent
Page 153: Figure 4.2.11 Samples and prominent
Page 157: Figure 4.2. 13 Samples and prominen
Page 168 and 169: It is difficult to differentiate be
Page 170 and 171: Figure 4.2.18 Weights ofvariables (
Page 172: Figure 42.19 Distribution ofsamples
Page 175 and 176: 5.1 SPATIAL DI STRIBUTION s. DISCUS
Page 177: f igure 5.1.1 Zones coinciding with
Page 180: f igure 5. 1.2 Average and range (
Page 184: Figure 5.1.4 Zones (clusters) in th
Page 187: Figure 5.1.5 Direction ofthe mean s
Page 191 and 192: The location ofthe third station at
Page 193: Figure 5.1.7 Station locations and
Page 197: Figure 5.1.8 Station locations and
Page 201 and 202: 5.1.4 and Section 4.1.2). This clus
Page 206: f igure 5.1.12 Drift card trajector
Page 209: Figure 5. t .13 Driftobject tracks
Page 212 and 213: In conclus ion. fluvial input of PA
Page 214: Figure 5.2. 1 Cloud ofsamples andpr
Page 217 and 218: increased amount oflight eas ily pe
Page 219: Figure 5.2.2 Cloud ofsamples and pr
Page 222: Figure 5.:!.3 Six clusters identifi
Page 225 and 226: mass balance calculations show that
Page 228 and 229: The processes ofdegradation might p
Page 230 and 231: Although less intensive than at Det
Page 232 and 233: The processes ofweathering do not s
Page 234 and 235: subzones ofinfluence was suggested.
Page 236 and 237: possesses similar isotopic composit
Page 238 and 239: fallout office soots as indicated b
Page 240 and 241: confined to the northern part ofthe
Page 243 and 244: Section 5.1); may still be affected
Page 245: their relative position with respec
Page 248 and 249: 5.3 A MODEL OF SOURCES, PATHWAYS. T
Page 251 and 252: originate from the Maumee River at
Page 253 and 254:
6. CONCLUSIONS The major conclusion
Page 255 and 256:
7. REFERENCES Abrajano T. A. Jr.•
Page 257 and 258:
Einsenreich S. J. and Strachan W. M
Page 259 and 260:
Lee R. F. and Takahashi M. ( 1977)
Page 261:
Sherrill T. W. and Saylor G. S. (19
Page 264:
8. APPENDICES 242
Page 270 and 271:
l' Appendix AS. Characteristic PAil
Page 272 and 273:
Appeodil: A1. The hyperbolic equati
Page 275:
... '"
Page 280 and 281:
Appeadil. 82. 1bc output of a princ
Page 284 and 285:
Appendix 84. The output o r a princ
Page 288:
Appendix C3 . The results ora local
show all

I'r - Memorial University of Newfoundland

Create successful ePaper yourself

Delete template?

Save as template?