| dc.contributor.author | Xie, Huixiang. | en_US |
| dc.date.accessioned | 2014-10-21T12:35:48Z | |
| dc.date.available | 1999 | |
| dc.date.issued | 1999 | en_US |
| dc.identifier.other | AAINQ49301 | en_US |
| dc.identifier.uri | http://hdl.handle.net/10222/55684 | |
| dc.description | The environmental importance of atmospheric carbon disulphide (CS 2) is recognised by its potential role as a major precursor of carbonyl Sulphide (OCS). The ocean is believed to emit CS2 to air, but large uncertainty may exist in the assessments of sea-to-air fluxes of this compound partly due to the meager database we currently have for CS2 in the ocean. This work is intended to re-assess the flux estimates and to identify and evaluate the potential Sources for Oceanic CS2. | en_US |
| dc.description | CS2 was measured in both the surface and subsurface waters during three cruises: two in the North Atlantic and one in the Pacific Ocean. All the investigated waters were supersaturated in CS2 relative to the atmosphere. Two distinct types of vertical profiles were observed: one in the cool waters of the North Atlantic, characterized by gradual reduction in CS2 with depth, and another in the warm waters of the North Pacific central are. showing the coexistence of subsurface CS2 and chlorophyll maxima. | en_US |
| dc.description | Solar UV-initiated photochemical reactions were identified as a significant source for oceanic CS2. The photo-production rate of CS2 is positively correlated with absorbance at 350 run, suggesting that the reactions are mediated by coloured dissolved organic matter. Laboratory irradiations confirmed that cysteine and cystine are efficient precursors of CS2 and that OH radicals are likely to be important intermediates. | en_US |
| dc.description | CS2 data were collected from axenic monocultures of six species of marine phytoplankton: Chaetoceros calcitrans, Phaeodactylum tricornutum, Phaeocystis sp., Porphyridium purpureum, Synechococcus sp. and Isochrysis sp. For a period of between two weeks and forty days, substantial accumulation Of CS2 was found in the cultures of C. calcitrans, P. tricornutum and Phaeocystis sp. C. calcitrans has a potential for CS2 production about 10 times higher than P. tricornutum or Phaeocystis sp. CS2 formation was strongly dependent on the growth stage of the cultured species. (Abstract shortened by UMI.) | en_US |
| dc.description | Thesis (Ph.D.)--Dalhousie University (Canada), 1999. | en_US |
| dc.language | eng | en_US |
| dc.publisher | Dalhousie University | en_US |
| dc.publisher | | en_US |
| dc.subject | Physical Oceanography. | en_US |
| dc.subject | Physics, Atmospheric Science. | en_US |
| dc.subject | Geochemistry. | en_US |
| dc.title | A study of the ocean source of carbon disulphide. | en_US |
| dc.type | text | en_US |
| dc.contributor.degree | Ph.D. | en_US |
