ANALYSIS AND DISTRIBUTION FEATURES OF BENZOTHIOPHENE IN SEDIMENTS OF NANSHA ISLANDS SEA AREA     

杨桂朋  张正斌  张建武  刘莲生 《中国海洋湖沼学报》1997,15(3):199-204

unomicrroNTherearereportedstudisoninorganicsulfurcomPoundsinrnarinesedtritS(Song,l99(),Stefan,l994),butfeWonorganicsulfurcomPounds.Itwasshownthatthroughoilspthe,mnoffandatmosphdriproasses,manyanthropogedcorganicsulfurcomP0undsrnaybethenspotalintothemarineenvirorstWheretheycanbeeventuallydePositalalongwithnatamlorganicstilfUrcomPoundsinseddritSraateSetal.,l979).ResearchesonorganicstilfurcomPoundsinrnarinesedirnentSareofpotentialenvirornnentalchdricalshoilicanceforhaherunderstandingofthege…  相似文献   

DIMETHYLSULFIDE IN THE SOUTH CHINA SEA   总被引：1，自引：0，他引：1  

杨桂朋  丛旭东  张正斌  赵伟 《中国海洋湖沼学报》2000,18(2):162-168

ＩＮＴＲＯＤＵＣＴＩＯＮＧｒｅａｔｅｆｆｏｒｔｓｗｅｒｅｄｅｖｏｔｅｄｒｅｃｅｎｔｌｙｔｏｓｔｕｄｙｉｎｇｄｉｍｅｔｈｙｌｓｕｌｆｉｄｅ(ＤＭＳ)ｄｉｓｔｒｉｂｕｔｉｏｎｉｎｓｅａｗａｔｅｒ,ａｓｉｔａｃｃｏｕｎｔｓｆｏｒｔｈｅｍａｊｏｒｐａｒｔｏｆｔｈｅｓｕｌｆｕｒｆｌｕｘｆｒｏｍｔｈｅｏｃｅａｎｓｔｏｔｈｅａｔｍｏｓｐｈｅｒｅ.Ｍｏｒｅｏｖｅｒ,ｉｔｓｏｘｉｄａｔｉｏｎｐｒｏｄｕｃｔｓｉｎｔｈｅａｔｍｏｓｐｈｅｒｅｍａｙｉｎｆｌｕｅｎｃｅｅｎｖｉｒｏｎｍｅｎｔａｌａｃｉｄｉｆｉｃａｔｉｏｎａｎｄ…  相似文献   

Multilayer distribution of carbon dioxide system in surface water of the Yellow Sea in spring     

宫海东  张正斌  张闯  刘莲生  邢磊 《中国海洋湖沼学报》2007,25(1):1-15

Surface water can be divided into three layers from top downward: surface microlayer (SML, thickness≤50 μm), subsurface layer (SSL, ≈25 cm) and surface layer (SL, 1–5m), among which the SML plays an important role on sea-air interaction because of its unique physical-chemical property. Carbon dioxide system including DIC (dissolved inorganic carbon), Alk (alkalinity), pH and pCO2 (partial pressure of CO2) in multilayered waters of the Yellow Sea was studied for the first time in March and May 2005. The results show that: DIC and Alk are obviously enriched in SML. The contents of DIC, Alk and pCO2 become lower in turn from SML, SSL to SL, higher in March and lower in May, whereas for pH it was opposite. The relationship between DIC and Alk is clearly positive, but negative between pH and pCO2. Meanwhile, pCO2 and temperature/salinity is also in positive relation, pCO2 decreases with latitude increase. DIC and Alk show a similar variation trend with the maximum at 02:00–03:00, but pH and pCO2 show an opposite pattern. In addition, the distribution patterns are similar to each other in the three layers. The Yellow Sea is shown to be a sink of atmospheric CO2 in spring by two methods: (1) comparing pCO2 in seawater and atmosphere; (2) turning direction of “pH-depth” curve. Calculation on the base of pCO2 data in SML in four models shows that carbon flux in spring in the area was about -6.96×106 t C.  相似文献   

Study on Dissolved Trace Metals in Sea Surface Microlayer in Daya Bay     

张正斌刘春颖  刘莲生于琳 王肇鼎 《中国海洋湖沼学报》2004,22(1):54-63

Glass-plate sampling during 1988- 1999 in Daya Bay and suitable corresponding analytical methods were used for the measurement of dissolved trace metals, dissolved organic carbon, biological oxygen demand, chemical oxygen demand, salinity of the sea surface mierolayer and subsurface water. Apparent enrichment mechanism and diurnal variation have been revealed for dissolved trace metals in the microlayer in Daya Bay. The more dissolved organic matter was enriched in the sea surface microlayer, the more dissolved trace metals were enriched in the layer. The organic matter played an important role in the enrichment process. The diurnal variations of dissolved trace metals showed that their concentration was apparently inversely related to the tide activity that the concentration was low during rising tide, but high during falling tide. The behavior of dissolved trace metals expressed by the diurnal variation was clearly opposite to that of salinity.  相似文献   

THE INTRINSIC ACIDITY CONSTANTS AND SPECIFIC SURFACE AREA OF MARINE SOLID PARTICLES I. A NEW METHOD     

王修林  张正斌  刘莲生  陈少华 《中国海洋湖沼学报》1991,(3)

This paper proposes a new method for determining the intrinsic acidity constants K and K The new method is a great improvement over the modified Langmuir plot method generally adopted in that determination of these constants is not dependent on the specific surface area S of the marine solid particles. The new method was used to determine K, K and S for the main inorganic components of marine solid particles, including illite, montmorillonite, kaolinite, goethite, y-AlOOH. amorphous ferric oxide, MnO2, manganite, SiO 2 and calcium carbonate, and can facilitate the study on the effect of solution constituents, solution temperature, ionic strength, etc. on the value of  相似文献   

THE EFFECT OF AMINO ACIDS ON COPPER (Ⅱ)-GOETHITE ION EXCHANGE IN SEAWATER     

王修林  张正斌  刘莲生 《中国海洋湖沼学报》1987,(2)

In seawater, aside from metal elements and suspended particles, organic substances amount to about 500-2,000 ug carbon/1[8], which is not neglegible in comparison with that of minor metal elements. But in the study of the interaction of the three constituents (metal elements, organics, and suspended particles), theeffect of organics in seawater on the surface reaction of metal element--suspended particles has usuallybeen neglected. Recent theoretical research[1,11] confirmed the importance of the effect of organics inseawater on the surface reaction of metal element--suspended particles. Generally, the effect of organicson the reaction of metal ions, especially Cu(II), on a solid surface is either promotive[2] or inhibitive[7,9]. So far the fact that organics cannot affect the surface reaction of Cu(II) ions on solids has not been reported in literature. Our experimental results showed that none of the amino acids in seawater affect Cu(II)-goethite ion exchange under certain experimental condition (such  相似文献   

Colloid‘s influences on microalgae growth as a potential environmental factor     

赵新淮张正斌  刘莲生 《中国海洋湖沼学报》2003,21(3):270-279

The role of colloid as “colloid pump”in the ocean is well known. The important influence of colloid in seawater on the growth of microalga was found in our 1999--2000 study. Colloid concentrates were obtained by employing a cross-flow filtration system to ultrafilter seawater(which had been pre-filtrated by 0.45 μm acetate cellulose membrane) successively with different membranes. Ultrafiltration retentions (we called them colloid concentrates) together with control sample (seawater without colloid) were then inoculated with two species of microalgae and cultivated in selected conditions. Monitoring of microalgae growth during cultivation showed that all colloid concentrates had obvious influence on the growth of the microalgae studied. Addition of Fe(OH)3 colloid or organic colloid (protein or carbohydrate) to the control sample enhanced the microalgae‘s growth.  相似文献   

STUDY ON THE ANALYSIS AND DISTRIBUTION OF DIMETHYL SULFIDE IN THE EAST CHINA SEA   总被引：6，自引：0，他引：6  

杨桂朋  张正斌  刘莲生  刘心同 《中国海洋湖沼学报》1996,14(2):141-147

A method is described for determining dimethylI sulfide (DMS) in seawater. DMS was first extractedfrom the seawater using organic reagent, then reverse-extracted by 5% HgCl2. In the laboratory DMS wasreleased by concentrated HCI and finally measured by GC-FPD. The limit of detection me O.05 ng ofS. Measurements of DMS along surface transects and on wtital profibe across the EaSt China Sca (Ers)continental sheif showed tha itS conodIations of S in the surface seawater ranged from 64-180 ng/L andthat itS vertical djstribuion was divided into 3 trpes. Model talculations of a stagnant film show a DMSflux of 10.6 umol/m_2d the air-sea inteIha.  相似文献   

The stepwise exchange action and steric hindrance effect of organic phenols on clays in seawater   总被引：4，自引：0，他引：4  

杨桂朋  张正斌 《中国海洋湖沼学报》1994,12(1):61-70

The exchange action of six types of organic phenols on clay surfaces in seawater is systematically studied in this work. The following significant conclusions are drawn from the experiments. (1) The interaction of organic phenols with montmorillonite, illite and kaolinite in seawater is monovalent anion exchage.(2) Their isotherms of stepwise exchage on clay surfaces belong to the Langmuir type or stepwise type.(3) The discovery of the"steric hindrance effects of stepwise exchange of organic phenols on clays surfaces", and revelation of an exchange mechanisrn diffeient from that in references are the greatest achieverments in this work.  相似文献   

Determination of apparent sampling thickness of sea surface microlayer   总被引：5，自引：0，他引：5  

李军  丁海兵  吴志坚  张正斌  刘莲生 《中国海洋湖沼学报》1998,16(2):177-182

IwrRODUtvIONTheseasurfacendcrolayer(SML)isathinair-seainterfacelayerwithphySical,chdricalandbiologicalproperties.OrganicmateriaIs,haceAnIs,nutrientS,particulatCrnat-terandplanktonaregenefallyenrichedintheSML(Hardy,JT.etal.,l98O,Wunams,P.M.etal.,1986).ThesamPlersforcolledingtheSMLwerernainlyglassplatespearvey,G.W.etal.,l972,l985;ZhangZhengbinetal.,l996),rotatingdrums(Harvey,G.W.,1966,Daumas,R.A.l976),screensgurmt,W.D.,l965,Piotrowicz,S.R.etal.,l972,Carison,D.J.,l982),funneIs…  相似文献