Gschwend%20thesis.pdf

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14 12 e \ 10 -c: a. " -ci ;: 8 e c: (/ e Q) .. 0 + e 0 a. c: 6 e 14 - a. .. _ .r Q) (/ - e / II e ri 4 12 j\ __ J 1 e i , \ e 2 î .-'~.\ \ i\ I · , i 'e/\ 10 II , I e-e_e e-e 9 ~ , , - , I , I I I e .. , , 8 " 0 i ' , , i ' ci i :: 3/77 , i , , I , , I , I , ""c e ' i ~ i , P. P 6 0 , .r Ó o."? i \ u , J3 , p- i , i , Po i , i 4 , 1 , A ,Po, ~ R ¡i \ , ''b a i b. 0" 't 't \ \ I \ P--o 2 6/77 9/77 121 77 \ I ~ ò-.¿ Date (month 1 year) 3178 6/78 o
-127- production by the plankton or may represent oxidation products of algal lipids. Potential precursors and a viable mechanism for chemical oxidation of algal fatty acids to C6-CiO aldehydes are described in detail in chapter 2 (figure 2-l2). A group of longer-chain aldehydes became particularly abundant during the phytoplankton bloom of February, 1978. These included Cl2 to Cl5 saturated and unsaturated aldehydes (figure 3-20). The bloom was more than 85% Thalassiosira nordenskioeldii as mentioned previously; thus it seemed likely that this diatom was the ultimate source of this material. Figure 3-21 demonstrates the correlation of these compounds with cell numbers of this diatom. Accordingly, pure cultures of this diatom were grown in the laboratory. 4 Cultures (1600 ml of ~ 3 x IO cells/ml in log phase growth) were extracted with CH2Cl2 after collection on a glass fiber filter, and the extract chromatographed. No evidence for the presence of any aldehydes could be found. Another culture was stripped directly as normal volatile analysis of water samples is performed, but no aldehydes were found by this approach. Finally, approximately 100 ml of CD seawater were added to a culture and incubated for two additional weeks (stationary phase). Stripping this cuI ture did not provide any aldehydes ei ther ~ Thus, it seems that the diatom does not produce the aldehydes directly. Possibly, zooplankton plays a role in aldehyde production. Another possibility is that photochemical oxidation (which cannot occur with the lights used to incubate algae) of algal metabolites produced the aldehydes. Also, a less abundant phytoplankton species may have released these compounds during the bloom. Dimethyl Polysulfides. Another group of compounds (figure 3-22) observed
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VOLATILE ORGANIC COMPOUNDS IN SEAWA
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-3- concentrations were observed to
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-5- analyses. Joy Geiselman collect
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Approval Page Abstract. . . Acknowl
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Figure 2-1 2-2 2-3 2-4 2-5 2-6 2-7
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-11- 4-5 O-xylene in Vineyard Sound
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-14- background ~ the next two chap
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-16- those at room temperature. On
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-18-. Table l-l. Ha logenated volat
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-zo- They found total n-alkanes (C6
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-2Z- alpha-pinene ( ~ ), and limone
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-24- Land animals also utilize vola
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-26- importance of transport mechan
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-28- Recently, methods have been de
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-30- Figure 2-1. Station locations
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-32- A third set of seawater sample
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-34- These analyses provided a lowe
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'" ~ ~ ~ o 500 TEMPERATURE (OC) 10
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SampIe station/ depth (m) Sargasso
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NOj (PM/kg) o 10 20 30 40 chI a (Pg
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Figure 2-4. -42- o 0 . o Sections s
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-44- Figure 2-5. Sections showing n
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-46- Figure 2-6. Sections showing o
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-48- Figure 2-7. Sections showing i
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-50- and l49 (M+41) ions in the CH4
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~ ~ ~ ~ ii "' ~ ï: "' l¡ Q: 3(' 5
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-54- A family of straight chain ald
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o 10 6 6.0 100 3.2 1000 . 2.2 0 9.2
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-58- Equatorial Atlantic, does not
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-60- Zsolnay (l973, 1976) has repor
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netS 40 (ng/kg) 20 +24/7 +15/7 30 2
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sample was enriched relative to adj
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-67- On the other hand, a phytoplan
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°2 (m//kg) 2 6 . . . . 4 . . . . .
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-71- Figure 2-13. Mechanism for pro
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-73- fatty acid, hexadecanoic acid,
Page 75 and 76: -75- In addition, the Cape, and the
Page 77 and 78: ::.',:.:' 71° 70° 69° 68° 67°W
Page 79 and 80: -79- Figure 3-2. Recirculating stri
Page 81 and 82: -81- o (heated to 60 C to reduce th
Page 83 and 84: VOLATILE EXTRACTION ref. Grab and Z
Page 85 and 86: RESULTS AND DISCUSSION Hydrographic
Page 88 and 89: -88- Figure 3-5. Salinity (0/00) ve
Page 90 and 91: -90- revealing the variation of sal
Page 92 and 93: .. 1.5 ..E0 1.0 - Ci ci :: 0.5 II'
Page 94 and 95: -94- Figure 3-7. Chlorophyll ~ (~g/
Page 96 and 97: -96- Three known incidents of hydro
Page 98 and 99: ~ ( ng/kg) 40 30 20 ._... ~ ? 1 0 .
Page 100 and 101: ~ 4 2 ( ng/kg) o '-+~ ( ng/kg) ~ (
Page 102 and 103: o to o (\ . -. /..., ., --. o .. (a
Page 104 and 105: -104- Figure 3-11. O-xylene concent
Page 106 and 107: -106- Figure 3-12. Electron impact
Page 108 and 109: -108- (Müller and Jaenicke, 1973).
Page 110 and 111: 30 20 UNKNOWN m.w. 108 10 (ng/kg) o
Page 112 and 113: -112- Figure 3-14. Naphthalene and
Page 114 and 115: -114- The naphthalene-to-methyl nap
Page 117 and 118: -117- with 0.29 for o-xylene and 0.
Page 119 and 120: nC14 15 10 (ng/kg) 5 o 80 60 n C 15
Page 121 and 122: "ep¡" 50 40 30 20 10 s...." . . \~
Page 123 and 124: -123- Figure 3-18. C6-CiO aldehyde
Page 125: Figure 3-19. -125- Heptanal concent
Page 129 and 130: 20 18 2 16 ~ "- 14 3 3 3 :- 12 3/ 2
Page 131 and 132: tf 10-' ~ ~ ct ~ ~ ~ ~ '" .. ~ ~ ~
Page 133 and 134: 15 DMDS (ng/kg) 5 o 35 30 25 DMTS 2
Page 135 and 136: -135- polysulfide volatiles. Partic
Page 137 and 138: TOTAL VC (ng/kg) 500 400 300 200 10
Page 139 and 140: -139- This suggested an anthropogen
Page 141 and 142: "Also, short range transport and de
Page 143 and 144: -143- were conducted. Rain samples
Page 145 and 146: Short-term Temporal Studies. -145-
Page 147 and 148: 40r RAIN RAIN 124 ~ 0 \ . MORNING (
Page 149 and 150: -149- Figure 4-2. Relative C2- and
Page 151 and 152: -151- Finally, the diesel-exhause-d
Page 153 and 154: Figure 4-3. Ratios of C2- and sampl
Page 155 and 156: Figure 4-4. Salini ty CD taken velo
Page 157 and 158: -157- Figure 4-5. O-xylene concentr
Page 159 and 160: -l59- while at other times they wer
Page 161 and 162: CDsw CDsw 11/10/77 11/22/77 CDsw 10
Page 163 and 164: -163- Figure 4-6. a-xylene concentr
Page 165 and 166: -165- The Quashnet River and Sippew
Page 167 and 168: Sippewissett Quashnet CD Marsh CD C
Page 169 and 170: r . I , , I . . I · ~_. . . TEMP .
Page 171 and 172: DATE AIR MEASUREMENTS -171- o-xylen
Page 173 and 174: -173- but that direct inputs (e.g.
Page 175 and 176: -175- an atmospheric source did not
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Table 5-1. Date of collection colle
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-179- gas chromatograph equipped wi
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-181- UCON R1 Compound SE54 R1 HB51
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Release rates (ng/gm dry weight/day
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- l86- are shown in parenthese s. T
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-l88- June and September, it may be
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-190- study in some summer samples
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-192- Surprisingly, the Rhodophyta
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-194- Three deep samples (ca. 2000m
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-196- indicated that these hydrocar
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-l98- average year-round sample dat
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-200- hydrogens of the C2- and C3-b
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-202- Application of sensitive sele
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-204- tubing into round bottom flas
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-206- Figure I-I. Stripper used wit
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-208- sample. Sample water was forc
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-ZIO- ionization spectra were acqui
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. . TEMP BLAN K BEFORE SAMPLE 10m 2
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-214- Table I-i. Recoveries (%) of
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-2l6- Table 1-2. Standard deviation
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Grob Methodology -2l8- The methods
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-220- compound m & p xylenes mw 108
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-222- Table 1-4. Recoveries (ng/kg)
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-224- purchased them. Tenax may be
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-226- Appendix II. Hydrographic dat
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-229- Appendix III. Volatile organi
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94 R. P. SCHWARZENBACH, R. H. BROMU
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96 R. P. SCHWARZENBACH. R. H. BROMU
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98 R. P. SCHWARZENBACH, R. H. BROMU
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100 R. P. SCHWARZENBACH, R. H. BRoM
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102 R. P. SCHWARZENBACH, R. H. BROM
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104 Oxygeii compouiids R. P. SCHWAR
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106 R. P. SCHWAKZENRACH. R. H. BROM
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-245- Appendix iv. Physical chemica
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-247- Appendix V. Mass spectra of s
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IS N L~ N r IS N ~Ð :i ,E -i Ji: "
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LD~ E) E) (Y E) LD E) LD N X E) in
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il .. E) N X I E) E) (Y E) il N E)
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CD CD .. r. L. - N ~-'._-----'-----
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E) i N f f ( -455 .- N ~ r t ì igN
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E) E) ~i !D i N --- J -lri r~ 18 r~
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REFERENCES Ackman, R.G., C. S. Toch
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. Cleveland, W. S., B. air pollutio
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-264- Grob, K. and F. ZUrcher. (l97
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-266- Lee, C. and J.L. Bada. (1975)
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-268- N. A. S. (1975a) Assessing Po
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-270- Strickland, J.D .R. and T .R.
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