This study on the sectional and vertical distribution of dissolved oxygen (DO) and the O<sub>2</sub> fluxes acrossthe sea-air interface in East China Sea (ESC) waters shows that the waters were in stea...This study on the sectional and vertical distribution of dissolved oxygen (DO) and the O<sub>2</sub> fluxes acrossthe sea-air interface in East China Sea (ESC) waters shows that the waters were in steady state and thatthe difference of DO was great in upper and bottom waters in Apr. 1994; but that seawater mixingwas strong and the difference of DO was small in upper and bettom waters in Oct. 1994. The above con-dusions were specially obvious in continental shelf waters under 100m. The DO maximum in subsurfacelayer waters appeared only at several stations and in general the DO in the waters decreased with depth.The horizontal distributions of O<sub>2</sub> fluxes across the sea-air interface appeared in stripes in Leg 9404 whenmost regions covend were supersaturated with O<sub>2</sub>. seawater to air flux wn large, and that on section No.1was 1.594 L/m<sup>2</sup>·d. The horizontal distribution of O<sub>2</sub> fluxes across the sea-air interface appeared lumpy inLeg 9410, when most regions covered were unsaturated with O<sub>2</sub>. O<sub>2</sub> was dissolved from展开更多
The optimum reaction conditions of the oxidative polycondensation of 2-(thien-2-yl-methylene)aminophenol (2-TMAP) has been accomplished by using air O_2,H_2O_2 and NaOCl oxidants in an aqueous alkaline medium between...The optimum reaction conditions of the oxidative polycondensation of 2-(thien-2-yl-methylene)aminophenol (2-TMAP) has been accomplished by using air O_2,H_2O_2 and NaOCl oxidants in an aqueous alkaline medium between 20℃and 90℃.The structures of the monomer and oligomer were confirmed by FT-IR,UV-Vis,~1H-NMR and ^(13)C-NMR and elemental analysis.TGA-DTA,size exclusion chromatography(SEC) techniques and solubility tests were applied for characterization.The ~1H-NMR and ^(13)C-NMR data show that the polymeriz...展开更多
文摘This study on the sectional and vertical distribution of dissolved oxygen (DO) and the O<sub>2</sub> fluxes acrossthe sea-air interface in East China Sea (ESC) waters shows that the waters were in steady state and thatthe difference of DO was great in upper and bottom waters in Apr. 1994; but that seawater mixingwas strong and the difference of DO was small in upper and bettom waters in Oct. 1994. The above con-dusions were specially obvious in continental shelf waters under 100m. The DO maximum in subsurfacelayer waters appeared only at several stations and in general the DO in the waters decreased with depth.The horizontal distributions of O<sub>2</sub> fluxes across the sea-air interface appeared in stripes in Leg 9404 whenmost regions covend were supersaturated with O<sub>2</sub>. seawater to air flux wn large, and that on section No.1was 1.594 L/m<sup>2</sup>·d. The horizontal distribution of O<sub>2</sub> fluxes across the sea-air interface appeared lumpy inLeg 9410, when most regions covered were unsaturated with O<sub>2</sub>. O<sub>2</sub> was dissolved from
基金supported by the Government Planning Organization(GPO2002K120170-7)TUBITAK GrantsCommission for a research grant(No.TBAG-105T428).
文摘The optimum reaction conditions of the oxidative polycondensation of 2-(thien-2-yl-methylene)aminophenol (2-TMAP) has been accomplished by using air O_2,H_2O_2 and NaOCl oxidants in an aqueous alkaline medium between 20℃and 90℃.The structures of the monomer and oligomer were confirmed by FT-IR,UV-Vis,~1H-NMR and ^(13)C-NMR and elemental analysis.TGA-DTA,size exclusion chromatography(SEC) techniques and solubility tests were applied for characterization.The ~1H-NMR and ^(13)C-NMR data show that the polymeriz...