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Figure 5.2.4 Station locations and major hydrocarbon reservoirs underlying the lake after Fuller and Shear (1995). Note that station 966 is situated within the oil field in the northern part<strong>of</strong> Western Basin.
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POLYCYCLIC AROMATIC HYDROCARBONS IN
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composition. Portions ofthe lake th
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TABLE OF CONTENTS . ABSTRAcr._._ _
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6. CONCLUSIONS_._ _....._._._ _ ._
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FIGURE 3.104 CONfIGURATION OF ISOCH
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FIGURE 4 .2.12 SAMPLES AND PROMINEN
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fIGURE 5.3.1 DESCR1Pl1VE MODEL OF S
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APPENDIX B 3 _ T HEoerwt Of A PtUNC
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Ip » Ideno(l,2.3 cd)pyrene NIST =
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Figure L 1.1 The 16 parental polycy
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After release by the primary source
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decomposition processes (O'Malley e
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Figure 2.1.1 The Great Lakes draina
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;: Duluth Chicago 1 J Lake Superior
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are the Black River, the Cuyaho ga
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Figure 1.1.5 The pattern of permane
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sedimentary basins, Western. Centra
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Figure 2. 1.8 Summer (July) air and
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Natural Resources: The lower Great
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American waters under the current U
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continuously overflowed com bined s
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3.1 EXPERIMENTAL 3. METHODS 3.1.1 S
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Table 3,1.1 Locations and types ofs
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Figure 3.12 Extraction and purifica
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hexane. 2) the unsaturated aliphati
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this problem. Ratios ofthe two stab
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Figure 3. 1.4 Configuration ofIsoch
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3.2.1 UNl- AND BIVAJUATE METHODS Th
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f igure 3.2. 1 Mean and range (± s
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utilized the same instrument (Isoch
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Selecting lIt1J'iahlu: It was demon
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w- _ 71
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seven variables with fewer missing
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analysis also employed a greate r n
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description. The second cluster ana
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elationships between different site
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Figure 4.1.3 Regression ofthree fir
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Figure 4.[.5 Isotopic composition (
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Figure 4.1.6 Weights ofvariables (c
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Figure 4.1.8 Distri bution ofsample
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those at the majority ofstations. S
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Ion, 969, 971, 357, 358). In additi
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Figure 4.2.3 Samples and prominent
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analysis supported some ofthc previ
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, ", Is , , >\ ryr " II ,- - , I ,
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11'
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sources (Fi g. 4.2 .5c). This compo
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Figure 4.2.7 The relative contribut
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".1.1.2 Miring CllrIIU (isotopic co
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Figure 42.9 Samples and promin ent
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Figure 4.2. 13 Samples and prominen
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It is difficult to differentiate be
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Figure 4.2.18 Weights ofvariables (
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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 204: Figure 5.1.1 1 Statioo locations an
Page 208 and 209: unaffected by the contaminated flow
Page 211 and 212: this station is die clo$esf to the
Page 213 and 214: samples and sources (Fig. 52.1 and
Page 216 and 217: There is yet another observation po
Page 218 and 219: with the relative contribution ofdi
Page 221 and 222: Table S.l.1 Six dusters identified
Page 224 and 225: the three previous ly identified zo
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: ... '"
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Appeadil. 82. 1bc output of a princ
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Appendix 84. The output o r a princ
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Appendix C3 . The results ora local
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