Environmental Engineering Reference
In-Depth Information
[3]
Berner R.A. and Canfield D.E. A model for atmospheric oxygen over phanerozoic time.
Am J Sci 1989; 289: 333-61.
[4]
Bezborodov A.A. and Eremeev V.N.
Chernoe more. Zona vzaimodeistviya aerobnikh I
anaerobnikh vod. (Black Sea. The oxic/anoxic interface)
, Sevastopol, MHI ASU, 1993.
(in Russian)
[5]
Brewer P.G. and Murray J.W. Carbon, nitrogen and phosphorus in the Black Sea. Deep-Sea
Res 1973; 20:803-18.
[6]
Broenkow W.W. and Cline J.D. Colorimetric determination of dissolved oxygen at low
concentrations. Limnol Oceanogr 1969; 14(3):450-54.
[7]
Buesseler K.O., Livingston H.D. and Casso S.A. Mixing between oxic and anoxic waters
of the Black Sea as traced by Chernobyl cesium isotopes. Deep-Sea Res 1991; 38:725-46.
[8]
Buesseler K.O., Livingston H.D., Ivanov L. and Romanov A. Stability of the oxic-anoxic
interface in the Black Sea. Deep-Sea Res I 1994; 41(2):283-96.
[9]
Caspers H. “Black Sea and Sea of Azov”. In
Treatise on marine ecology and paleoecology
.
Hedgpeth J.W. ed., Geological Society of America Memoirs, 1957.
[10]
Codispoti L.A., Friederich G.E., Murray J.W. and Sakamoto C.M. Chemical variability
in the Black Sea: implication of continuous vertical profiles that penetrated oxic/anoxic
interface. Deep-Sea Res 1991; 38(2):691-710.
[11]
Debol'skaya E.I. and Yakushev E.V. The role of suspended manganese in hydrogen sulfide
oxidation in the Black Sea redox-zone. Water Resources 2002; 29:72-77. (In Russian)
[12]
Dyrssen D. Metal complex formation in sulphidic seawater. Mar Chem 1985; 15:285-93.
[13]
Dyrssen D., Haraldsson C., Westerlund S. and Aren K.
Report on the Chemistry of
seawater, XXXII. Department of Analytical and Marine Chemistry
, Chalmers University
of Technology and university of Goteborg, Goteborg, Sweden, 1986.
[14]
Fonselius S.H. “Phosphorus in the Black Sea.” In
The Black Sea - Geology, Chemistry
and Biology.
Degens E.J., Koss D.A. eds., Amer Ass of Petrol Geologists Tulsa, 1974.
[15]
Fuchsman C.A. and Murray J.W. Nitrogen species concentration and natural stable isotope
profiles of the Black Sea. Deep-Sea Res Pt II, submitted.
[16]
Goyet C., Bradshaw A.L. and Brewer P.G. The carbonate system in the Black Sea. Deep-
Sea Res 1991; 38:1049-68.
[17]
Gregg M.C. and Yakushev E. Surface ventilation of the Black Sea's cold interme-
diate layer in the middle of the western gyre. Geophys Res Lett 2005; 32:L03604,
doi:10.1029/2004GL021580.
[18]
Gunnerson C.G. and Ozturgut E. “The Bosporus.” In
The Black Sea-geology, chemistry
and biology.
Degens E.T. and Ross D.A. eds., AAPG, Memoir 20, 1974.
[19]
Holland H.D.
The Chemical Evolution of the Atmosphere and Oceans.
Princeton Univ.
Press, Princeton, 1984.
[20]
Humborg C., Ittekkot V., Cociasu A. and v.Bodungen B. Effect of Danube River dam on
Black Sea biogeochemistry. Nature 1997; 386:385-88.
[21]
Ivanov L.I., Konovalov S.K., Belokopytov V. and Ozsoy E. “Regional peculiarities of
physical and chemical responses to changes in external conditions within the Black Sea
pycnocline: cooling phase.” In
NATO ASI Series. NATO TU-Black Sea project: Ecosystem
modelingasamanagementtoolfortheBlackSea.Symposiumonscientificresults.
Ivanov
L. and Oguz T. eds., Kluwer Academic Publishers, The Netherlands, 1998.
