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chinese Science Bulletin 2000年第S1期45卷 26-34页

作者： wang yunpengguangzhou institute of geochemistry, chinese academy of sciences, guangzhou 510640, china guangzhou institute of geochemistry Chinese Academy of Sciences Guangzhou China

This paper presents the contents of 17 kinds of trace elements in plant leaf samples collected from 4 sections in the North Jiangsu oil field, and the dada on their visible-near infrared spectra. By comparing the results of the inner and outer oil-gas remote-sensing anomaly areas, the plant trace element composition, and the enrichment characteristics and their influence on the plant spectral properties are described. The results indicated that the plant leaves had very strong enrichment ability toward some elements such as Mg, Ca, K, Na, Fe, Al, Mn, V, Zn and Cr. The plant leaves from the oil-gas abnormal areas were enriched in trace elements of the Fe-series, but depleted in alkali and alkali-earth metal elements. The plant trace elements had a strong influence on the 'blue-shift' strength and the reflectance of visible bands. And the ratios between Fe, Co and K, Na, Cd, Cu, Ba are the effective remote-sensing oil-indicating factors of plant trace elements. plant trace element, geochemistry, remote

关键词： plant trace element geochemistry remote sensing spectra North Jiangsu oil fleld.

The non-point source (NFS) information system based on remote sensing and GIS and its preliminary application

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chinese Science Bulletin 2000年第S1期45卷 71-75,116页

作者： wang yunpengguangzhou institute of geochemistry, chinese academy of sciences, guangzhou 510640, china

A non-point source information system (NPSIS) has been constructed by use of remote sensing and GIS technology, and a construction method of NPSIS introduced with Shenzhen as an example. With the remote sensing land-using images as an environment unit, the analysis modules based on NPSIS are built through combining the NPS model with NPSIS, and the preliminary NPS calculation and analysis performed.

关键词： remote sensing GIS non-point source NPS information system.

Nitric Oxide Emission Following Wetting of Dry Soils in Subtropical Humid Forests

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Pedosphere 2009年第6期19卷 692-699页

作者： LI De-Jun and wang Xin-Ming 2 State Key Laboratory of Organic geochemistry, guangzhou institute of geochemistry, chinese academy of sciences, guangzhou 510640 (china) State Key Laboratory of Organic geochemistry Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou 510640 (China)

Information about soil nitric oxide （NO） emissions from subtropical forests is quite limited, and even less is known about the pulse emission of NO when wetting soils after a long period of dryness. In this study, we measured NO fluxes following wetting of dry soft in a broadleaf forest and a pine forest in subtropical china. Large pulses of NO fluxes were observed after soil wetting in both forests. NO fluxes increased significantly within 0.5 h following wetting in both forests and reached peak 1 and 4 h after soil wetting in the pine forest and the broadleaf forest, respectively. In the broadleaf forest, averaged peak flux of NO pulses was 157 ng N m^-2 s^-1, which was 8 times the flux value before wetting, and in the pine forest, the averaged peak flux was 135 ng N m-2 s 1, which was 15.5 times the flux value before wetting. The total pulses-induced NO emissions during the dry season were roughly estimated to be 29.4 mg N m^-2 in the broadleaf forest and 22.2 mg N m^-2 in the pine forest or made up a proportion of 4.6% of the annual NO emission in the broadleaf forest and 5.3% in the pine forest.

关键词： dry season flux. NO. pulse subtropical china

^(40)Ar/^(39)Ar chronology and geochemistry of high-K volcanic rocks in the Mangkang basin, Tibet

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Science china Earth sciences 2005年第1期48卷 1-12页

作者： ZHANG Huihua, HE Huaiyu, wang Jianghai & XIE Guanghong guangzhou institute of geochemistry, chinese academy of sciences, guangzhou 510640, china institute of Geology and Geophysics, chinese academy of sciences, Beijing 100029, china College of Life sciences, Sun Yat-Sen University, guangzhou 510275, china chinese academy of sciences Guangzhou Institute of Geochemistry Guangzhou China chinese academy of sciences Institute of Geology and Geophysics Beijing China College of Life sciences Sun Yat-Sen University Guangzhou China

Our two newly obtained high-quality 40Ar/39Ar ages suggest that the high-K volcanic rocks of the Lawuxiang Formation in the Mangkang basin, Tibet were formed at 33.5 ( 0.2 Ma. The tracing of elemental and Pb-Sr-Nd isotopic geochemistry indicates that they were derived from an EM2 enriched mantle in continental subduction caused by transpression. Their evidently negative anomalies in HFSEs such as Nb and Ta make clear that there is an input of continental material into the mantle source. The high-K rocks at 33.5 ( 0.2 Ma in the Mangkang basin may temporally, spatially and compositionally compare with the early one of two-pulse high-K rocks in eastern Tibet distinguished by wang J. H. Et al., implying that they were formed in the same tectonic setting.

关键词： Cenozoic high-K volcanic rocks, 40Ar/39Ar chronology, Mangkang basin, Tibet.

Noble gas and cosmic-ray exposure age of Juancheng chondrite

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chinese Science Bulletin 1999年第12期44卷 1142-1143页

作者： wang Daode and wang Ruitian guangzhou institute of geochemistry, chinese academy of sciences , guangzhou 510640, china Heze Bureau of Seismology, Shandong Province , Heze 274026, china guangzhou institute of geochemistry Chinese Academy of Sciences Guangzhou China Heza Bureau of Seismology Shandong Province Heze China

The analytical results of noble gase in recently fallen Juancheng chondrite indicate that cosmic-ray ages of cosmogenic nuclei of 3He, 21Ne and 38Ar are 5.1, 5.0 and 5.8 Ma, respectively, averaging 5.3 Ma. The gas retention ages radiogenic nuclei of 4He and 40Ar are 3200 and 4 200 Ma, respectively. The average cosmic-ray age shows that it has occurred at breakup of the meteoroid from its parent body by impact before 5.3 Ma.

关键词： noble gas cosmic-ray exposure age chondrite Juancheng Shandong.

The biomarkers of 2,6,10,15, 19-pentamethylicosenes and their carbon isotopic composition in the sediments from the Gulf of Mexico

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chinese Science Bulletin 2006年第14期51卷 1736-1740页

作者： SONG Zhiguang1,2 & wang Cuiping1,31. State Key Laboratory of Organic geochemistry, guangzhou institute of geochemistry, chinese academy of sciences, guangzhou 510640, china 2. guangzhou Research Center of Gas Hydrate, chinese academy of sciences, guangzhou 510640, china 3. Graduate School of chinese academy of sciences, Beijing 100039, china State Key Laboratory of Organic geochemistry Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou China guangzhou Research Center of Gas Hydrate Chinese Academy of Sciences Guangzhou China Graduate School of chinese academy of sciences Beijing China

A group of 2,6,10,15,19-pentamethyli- cosenes (PMIΔ) containing 1―5 unsaturated double bonds has been identified in the sea floor sediments from the Gulf of Mexico at the Green Canyon 238 *** PMIΔ compounds are distributed between nC22 and nC24 on the mass chromatogram of aliphatic fraction. Their δ 13C values are very much depleted in 13C and in the range of ?86.7‰ to ?115.5‰, whereas the δ 13C values of companion n-alkanes range from ?28.4‰ to ?34.6‰. These unsaturated PMIΔ com-pounds are typical biomarkers derived from the an-aerobic oxidation of methane mediated by meth-ane-oxidizing archaeal bacteria and indicative of the gas seeps or even the occurrence of gas hydrates in the deep sea sediments.

关键词：生物标志墨西哥湾沉积物 PMIA 天然气水化物

Alkalic-type epithermal gold mineralization associated with Tongshi complex in Pinyi County, Shandong Province

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chinese Science Bulletin 1999年第S2期44卷 236-238页

作者： XIONG Xiaolin, ZHAO Zhenhua and wang Qiang guangzhou institute of geochemistry, chinese academy of sciences, guangzhou 510640, china guangzhou institute of geochemistry Chinese Academy of Sciences Guangzhou 510640 China

THE alkali-rich subvolcanic complex of Tongshi and the associated gold mineralization are located at thesouth boundary of Pinyi Mesozoic volcanic depression in western Shandong Province. There are morethan 30 gold deposits and mineralization locations around the complex, in which Guilaizhuang gold deposit and Zhuojiazhuang bonanza gold deposit with important economic value are included. This area isbecoming a perspective target of superlarge gold deposit. In the mine area, there crop out Archeangranitic gneisses, Paleozoic carbonates and Jurassic clastic rocks, which was intruded by Tongshi complexwith 30 km. The complex consists of K-high igneous rocks formed by two stages of magmatism. In thefirst stage, the monzonitic dioritic porphyrys, which belong to K-high calc-alkalic rocks, were formed andin the second stage, monzonitic-syenitic porphyrys, which belong to K-high alkalic rocks, were *** Ar-Ar ages are 189 Ma and 188 Ma, respectively. At the end of the second stage, a lot of theexplosive breccias were formed. The gold mineralization in this area is closely associated in time andspace with the second stage monzonitic-syenitic porphyrys. Based on the characteristics of

关键词： epithermal gold mineralization Tongshi complex Pinyi County Shandong Province.

Neutron capture effects and pre-atmospheric sizes of meteoroids

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chinese Science Bulletin 2003年第20期48卷 2236-2240页

作者： wang Daode & LIN Yangting guangzhou institute of geochemistry, chinese academy of sciences, guangzhou 510640, china Correspondence should be addressed to wang Daode (e-mail: gzwangdd @***) guangzhou institute of geochemistry Chinese Academy of Sciences Guangzhou 510640 China

Excesses of 80Kr and 82Kr, produced by secondary neutron capture effects of 79Br and 81Br, were observed in meteorites. Epithermal neutron flux, Jn (30—300 eV), and fast neutron flux, Jn( > 5 MeV), were determined according to reactions of 79Br(n, gb)80Kr, 81Br(n, gb)82Kr, and 24Mg(n, a)21Ne, respectively. Cosmogenic noble gases of several ordinary chondrites fell in china indicate a positive relationship between Jn (30—300 eV)/Jn ( > 5 MeV) ratio and Jn (30—300 eV). This suggests large pre-atmospheric sizes of the meteorites, and a considerable fraction of the secondary neutrons were slowed down to epithermal energy. According to its relationship with Jn (30—300 eV)/Jn ( > 5 MeV) ratio, the pre-atmospheric minimum radii and masses of several chinese chondrites were estimated as below: Zhaodong: 60 cm, 3200 kg; Laochengzhen: 23 cm, 490 kg; Suizhou: 31 cm, 450 kg; Xi Ujimgin: 22 cm, 160 kg; Dongtai: 21 cm, 140 kg.

关键词：流星体陨星中子俘获大气层前尺寸宇宙成因核素

Evaluation criteria for gas source rocks of marine carbonate in china

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Progress in Natural Science:Materials International 2005年第9期15卷 810-817页

作者： wang Zhaoyun1**, ZHAO Wenzhi1 and wang Yunpeng2(1. Research institute of Petroleum Exploration & Development,Petrochina, Beijing 100083, china 2. guangzhou institute of geochemistry, chinese academy of sciences, guangzhou 510640, china) Research institute of Petroleum Exploration and Development PetroChina Beijing 100083 China guangzhou institute of geochemistry Chinese Academy of Sciences Guangzhou 510640 China

Hydrocarbon generating and expulsion simulation experiments are carried out using samples artifically matched between the acid-dissolved residue of relatively low-maturity limestone and the original sample. This work makes up for the insufficiency of source rock samples with high abundance of organic matters and low maturity in china. The organic carbon content of the 10 prepared samples varies between 0.15% and 0.74%. Pyrolysis data and simulation experiment results of hydrocarbon generating and expulsion, which were obtained by a high-temperature and high-pressure open system, indicate that the lower limit of organic carbon content for marine carbonate rock to generate and expel hydrocarbons is 0.23%—0.31%. In combination with the numerical analysis of organic carbon in marine carbonate rocks from Tarim Basin, Sichuan Basin, Ordos Basin and North china, as well as the contribution of these gas source rocks to the discovered gas pools, we think that the organic carbon criterion for carbonate gas source rocks should be 0.3%.

关键词： carbonate gas source rock gas-generating efficiency evaluation criteria simulation experiment.

Ecology of the rehabilitation of vegetation on tropical coastal eroded land in Guangdong， china

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Journal of Environmental sciences 1995年第1期7卷 74-84页

作者： Yu Zuoyue wang Zhuhao South china institute of Botany, chinese academy of sciences,guangzhou 510650,china South china Inst of Botany Chinese Academy of Science Guangzhou China

ＥｃｏｌｏｇｙｏｆｔｈｅｒｅｈａｂｉｌｉｔａｔｉｏｎｏｆｖｅｇｅｔａｔｉｏｎｏｎｔｒｏｐｉｃａｌｃｏａｓｔａｌｅｒｏｄｅｄｌａｎｄｉｎＧｕａｎｇｄｏｎｇ，ＣｈｉｎａＹｕＺｕｏｙｕｅ；ＷａｎｇＺｈｕｈａｏＳｏｕｔｈＣｈ... 详细信息

ＥｃｏｌｏｇｙｏｆｔｈｅｒｅｈａｂｉｌｉｔａｔｉｏｎｏｆｖｅｇｅｔａｔｉｏｎｏｎｔｒｏｐｉｃａｌｃｏａｓｔａｌｅｒｏｄｅｄｌａｎｄｉｎＧｕａｎｇｄｏｎｇ，ＣｈｉｎａＹｕＺｕｏｙｕｅ；ＷａｎｇＺｈｕｈａｏＳｏｕｔｈＣｈｉｎａＩｎｓｔｉｔｕｔｅｏｆＢｏｔ...

关键词： tropics ereded land ecology of vegetation recovery.