Huang Xiaolong, Zhou Chunmei, Zhuang Youxiang, et al. Chart of Nuclide (2000)[DB/OL]∥Modified by Xiaoyz, October 2001[2005-12-05]. http:∥rsh.nst.pku.edu.cn/nuclide/.
[2]
Lal D, Somayajulu B L K. Some aspects of the geochemistry of silicon isotopes[J]. Tectonophysics, 1984, 105(1-4): 383-397.
[3]
王佩仪,晁念英,万军伟. 放射性同位素32Si及其研究进展[J]. 地质科技情报,1995,14(4):93-99. Wang Peiyi, Chao Nianying, Wan Junwei. The research advance in radioisotope silicon-32[J]. Geological Science and Technology Information, 14(4): 93-99 (in Chinese ).
[4]
Lindner M. New nuclides produced in chlorine spallation[J]. Physical Review, 1953, 91: 642.
[5]
Lal D, Goldberg E D, Koide M. Cosmic-ray-produced silicon-32 in nature[J]. Science, 1960, 131 (3397): 332-337.
[6]
Morgenstern U, Fifield K L, Zondervan A. New frontiers in glacier ice dating: Measurement of natural 32Si by AMS[J]. Nuclear Instruments and Methods in Physics Research B, 2000,172: 605-609.
[7]
Craig H, Somayajulu B L K, Turekian K K. Paradox lost: silicon 32 and the global ocean silica cycle[J]. Earth and Planetary Science Letters, 2000, 175: 297-308.
[8]
Morgenstern U, Toylor C B, Parrat Y, et al.32Si in precipitation: evaluation of temporal and spatial variation and as dating tool for glacial ice[J]. Earth and Planetary Science Letters, 1996, 144: 289-296.
[9]
Turkevich A, Samulels A. Evidence for32Si a long lived beta emitter[J]. Phys Rev 2nd Ser, 1954, 94:364.
[10]
Geithoff D. Uber die Herstellung von Si-32 durch einen (t, p)-Prozess[J]. Radiochimica Acts, 1962, 1: 3-6.
[11]
Honda M, Lal D. Spallation cross sections for long-lived radionuclides in iron and light nuclei[J]. Nuclear Physics, 1964, 51: 363.
[12]
Brodzineki R L, Finkel J R, Conway D C. β-spectrum of32Si[J]. Joural of Inorganic Nuclear Chemistry, 1964, 26: 677-681.
[13]
Jantasch K. Kernreaktionen mit tritonen beim 30Si: bestimmung der halbwertzeit von32Si[J]. Kernenergie, 1967, 10(3): 89.
[14]
Lal D, Nijampurkuar V N, Somayajulu B L K. Concentrations of cosmogenic32Si in deep Pacific and Indian waters based on study of galathea deep sea siliceous sponges[J]. Calathea Rep,1970, 2: 247.
[15]
Clausen H B. Dating of polar ice by32Si[J]. Joural of Glacialogy, 1973, 12: 411.
[16]
DeMaster D J. The half-life of32Si a varved Gulf of California sediment core[J]. Earth and Planetary Science Letters, 1980a, 48: 209-217.
[17]
Kutschera W, Henning W, Paul M, et al. Measurement of the32Si half-life via accelerator mass spectrometry[J]. Physics Review Letters, 1980, 45: 592-596.
[18]
Elmore D, Anantaraman N, Fulbright H W, et al. Half-life of 32Si from tandem-accelerator mass spectrometry[J]. Physics Review Letters, 1980, 45: 589-592.
[19]
Brzezinski M A, Phillips D R. Evalution of32Si as a tracer for measuring silica production rates in marine waters[J]. Limnology and oceanography, 1997, 42(5): 856-865.
[20]
Alburger D E, Harbottle G, Norton E F. Half-life of 32Si[J]. Earth and Planetary Science Letters, 1986, 78(2-3): 168-176.
[21]
Hofmann H J,Bonani G, Suter M, et al. A new determination of the half-life of32Si[J]. Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms, 1990, 52: 544-551.
[22]
Somayajulu B L K, Lal D, Craig H. Silicon-32 profiles in South Pacific[J]. Earth and Planetary Science Letters, 1973, 18(2): 181-188.
[23]
Thomsen M S, Heinemeier J, Hornsh J P, et al. Half-life of32Si measured via accelerator mass spectrometry[J]. Nuclear Physics A, 1991, 534(2): 327-338.
[24]
Chen Y, Kashy E, Benenson W, et al. Half-life of 32Si[J]. Physical Review C, 1993, 47(4): 1462-1465.
[25]
Nijampurkar V N, Rao D K, Oldfied F, et al. The half-life of Si-32: a new estimate based on varied lake sediments[J]. Earth and Planet Science Letters, 1998, 163: 191-196.
[26]
Lal D. New neclear methods for studies of soil dynamics utilizing cosmic ray produced radionuclides[C/OL]∥Stott D E, Mohtar R H,Steinhardt G C, et al. 2001. Sustaining the Global Farm. Selected paper from the 10th International Soil Conservation Organization Meeting held May 24-29, 1999 at Purdue University and the USDA-ARS National Soil Erosion Research Laboratory[2005-10-05]. http:∥topsoil.nserl.purdue.edu/nserlweb/isco99/pdf/ISCOdisc/Sustaining The Global Farm/P108-D%20Lal. pdf.
[27]
DeMater D J. Particle mixing rates and fluxs of dissolved silica from deep-sea baed on32Si measurement[J]. EOS, 1980b, 61: 269.
[28]
DeMaster D J, Cochran K J. Particle mixing rates in deep-sea sediments determined from excess 210Pb and32Si profile[J]. Earth and Planetary Science Letters, 1982, 61: 257-271.
[29]
Morgenstern U, Geyh M A, Kudras H R, et al.32Si dating of marine sediments from Bangladesh[J]. Radiocarbon, 2001, 43 (2B): 909-916.
[30]
宋燕,季劲钧,王月宾,等. 小冰期气候研究回顾和机理探寻[J]. 气象,2003,29(7):3-7. Song Yan, Ji Jinjun, Wang Yuebin, Wang Peitao. Reviews on Little Ice Age climate and approach to its mechanim[J]. Meteorology, 2003, 29(7): 3-7. (in Chinese).
[31]
李明启,靳鹤龄,张洪. 小冰期气候的研究进展[J]. 中国沙漠,2005,25(5):731-737.Li Mingqi, Jin Heling, Zhang Hong, Advances of climate research in the Little Ice Age[J]. Journal of Desert Research, 2005, 25(5): 731-737(in Chinese ).
[32]
郑景云,王绍武. 中国过去2000年气候变化的评估[J]. 地理学报,2005,60(1):21-31. Zheng Jingyun, Wang Shaowu.Assessment on climate in China for the last 2000 years[J]. Acta Geographica Sinica, 2005, 60(1): 21-31(in Chinese ).
[33]
陈星,刘健,王苏民. 东亚地区小冰期气候的模拟[J]. 气象科学,2005,25(1):1-8. Chen Xing, Liu Jian, Wang Suimin. Climate simulation of Little Ice Age over Eastern Asia[J]. Scientia Meteorologica Sinica, 2005, 25(1): 1-8(in Chinese ).
[34]
Einloth S, Ekwurzel B, Eastoe C, et al. Progress on the Development of32Si as a Potential Tracer for Centuryscale Recharge in Semi-arid Regions [C/OL][20051005]. http:∥www.sahra.arizona.edu/events/meetings/2002annmeeting/posters/Einloth Sharon-Si32.pdf.
[35]
Dansgaar W, Clausen H B. Evidence for bomb-produced silicon-32[J]. Journal of Geophysical Research, 1966, 71(22): 5474-5476.
[36]
Lal D, Nijampurkar V N, Rajagopalan G. Annual fallout of32Si, 210Pb, 22Na, 35S and 7Be in rain in India[J]. Proc. Indian Acad Sci, 1979, 88a: 29-40.
[37]
Kharkar D P, Nijampurkar V N, Lal D. The goble falloutof32Si produced by cosmic rays[J]. Geochimica et Cosmochimica Acta, 1966, 30: 621-631.
[38]
Lal D, Peters B. Cosmic ray produced radioactivity on the earth[J]. Handb Physik, 1967, 46: 551-612.
[39]
Franke T, Frohlic K, Gellermann R, et al.32Si in precipitation of Freiberg (GDR)[J]. J Radioanal Nucl Letters, 1986, 103(1): 11-18.
[40]
Somayayjulu B L K, Rengarajan R, Lal D, et al. GEOSECS Atlantic32Si Profiles[J]. Earth and Planetary Science Letters, 1987, 85: 329-342.
[41]
Somayayjulu B L K, Rengarajan R, Lal D, et al. GEOSECS Pacific and India Ocean32Si Profiles[J].Earth and Planetary Science Letters, 1991, 107: 197-216.
[42]
Fairbridge R W. The Encyclopedia of Geomorphology[M]. New York: Reinhold, 1968: 177-186.
[43]
Nijampurkar V N, Rao D K. Polar fallout of radionuclides32Si, 7Be, and 210Pb and past accumulation rate of ice at Indian station, Dakshin Gangotri, East Antarctica[J]. Jounal of Environmental Radioactivity, 1993, 21: 107-117.
[44]
Treguer P, Nelson D M, Van Bennekom A J, et al. The scilica balance in the world ocean: A reestimate[J]. Science, 1995, 268: 375-379.
[45]
Treguer P, Lindner L, Van Bennekom A J, et al. Production of biogenic silica in the Weddel-Scotia Seas measured with32Si[J]. Limnology and Oceanography, 1991, 36 (6): 1217-1227.
[46]
Susan M L. An Introduction to Marine Biogeochemistry[M]. New York: John Wiley & Sons, Inc., 1992.
[47]
Einloth S, Ekwurzel B, Eastoe C, et al. 32Si as a potential tracer for centuryscale recharge in semiarid regions[C/OL]∥ Geophysical Research Abstracts, 2003, 5: 13164[2005-10-05]. http:∥www.sahra.arizona.edu/events/meetings/2002_ann_ meeting/posters.html,.
[48]
Lal D, Nijampurkar V N, Somayayjulu B L K, et al. Silicon-32 specific activities in coastal waters of world oceans[J]. Limnology and Oceanography, 1976, 21(2): 285-293.
[49]
Lal D, Somayaju B L K. 1980. 利用宇宙成因的32Si研究近岸水体的混合作用的可能性[M]∥戈德堡[美],掘部纯男[日],猿桥藤子[日]. 黄奕普,施文远,邹汉阳,等译. 同位素海洋化学. 北京:海洋出版社,1990:90-97.
[50]
Peng T H, Maier-Reimer E, Broecker W S. Distribution of32Si in the world ocean: model compared to observation[J]. Global Biogeochemical Cycles, 1993, 7: 463-474.
[51]
Nijampurkar V N, Martin J M, Meybeck M. Silicon-32 as a tool for stufying silicon behaviour in estuaries[J]. Limnology and Oceanography, 1983, 28: 1237-1242.
[52]
Fifield L K, Morgenstern U. Silicon-32 as a tool for dating the recent past[J]. Quaternary Geochronology, 2009, 4: 400-405.
[53]
Kharkar D P, Lal D, Somayayjulu B L K. Investigations in marine environments using radioisotope produced by cosmic rays[C]∥ Proc. Int. Symp. Radioactive Dating. Athens: IAEA, 1963: 175-187.
[54]
Kharkar D P, Turekian K K, Scott M R Comparison of sedimentation rates obtained by32Si and uranium decay series determinations in some siliceous Antarctic core[J]. Earth and Planetary Science Letters, 1969, 6: 61-68.
Krishnawamy S, Lal D, Martin J M, et al. Geochronology of lake sediments[J]. Earth and Planetary Science Letters, 1971, 11(1-5): 407-414.
[57]
Martin J M, Meybeck M, Nijampurkar V N, et al. 210Pb, 226Ra and 32Si in Pavin lake (Masif Central, France)[J]. Chemical Geology (Isotope Geoscience Section), 1992, 94: 173-181.
[58]
Geyh M A. Symbiosis between geochronologists and quaternary geoscientists[J]. Geochronometria, 2001, 20: 1-8.
[59]
Brzeinski M A, Nelson D M. Seasonal changes in the silica cycle within a Gulf Stream warm-core ring[J]. Deep Sea Research, 1989, 36: 1009-1030.
[60]
Quéguinera B, Treguer P, Nelson D M. The production of biogenic silica in the Weddlell and Scotia Seas[J]. Marine chemistry, 1991, 35: 449-459.
[61]
De La Rocha C L, Brzezinski M A, DeNiro M J. Purification, recovery, and laser-driven fluorination of silicon from dissolved and particulate silica for the measurement of natural stable isotope abundances[J]. Analyt Chem, 1996, 68: 3746-3750.
[62]
Ragueneau O, Treguer P, Leynaert A, et al. A review of the Si cycle in the modern ocean-recent progress and mising gaps in the application of biogenic opal as paleoproductivity proxy[J]. Global and Planetary Change, 2000, 26: 317-365.
[63]
Bidle K D, Brzezinski M A, Long R A, et al. Diminished efficiency in the ocean silica pump caused by bacteria mediated silica dissolution[J]. Limnology and Oceanography, 2003, 48(5): 1855-1868.
[64]
Brown L, Sanders R, Saidge G, et al. The uptake of silica during the spring bloom in the Northeast Atlantic Ocean[J]. Limnology and Oceanography, 2003, 48(5): 1831-1845.
[65]
Leynaert A, Tréguer P, Lancelot Christiane,et al. Silicon limitation of biogenic silica production in the Equatorial Pacifc[J]. Deep-Sea Research I, 2001, 48: 639-660.
[66]
Nelson D M, Brzezinski M A, Sigmon D E, et al. A seasonal progression of Si limitation in the Pacific sector of the Southern Ocean[J]. Deep Sea Research Part II: Topical Studies in Oceanography, 2001, 48 (1920): 3973-3995.
[67]
Franck V M, Brzezinski M A, Coale K H, et al. Iron and silicic acid concentrations regulate Si uptake north and south of the Polar Frontal Zone in the Pacific Sector of the Southern Ocean[J]. Deep Sea Research II: Topical Studies in Oceanography, 2000, 47(15-16): 3315-3338.
[68]
Blain S, Leynaert A, Tréguer P B. growth rate and limitation of Equatorial Pacific diatoms[J]. Deep-Sea ResearchⅠ, 1997, 44 (7): 1255-1275.
[69]
Popplewell J F, King S J, Day J P, et al. Kinetics of uptake and elimination of silicic acid by a human subject: a novel application of 32Si and accelerator mass spectrometry[J]. Journal of Inorganic Biochemistry, 1998, 69 (3): 177-180.
[70]
Ragueneau O, Lancelot C, Egorov V, et al. Biogeochemical Transformations of Inorganic Nutrients in the Mixing Zone between the Danube River and the North-western Black Sea[J]. Estuarine, Coastal and Shelf Science, 2002, 54 (3): 321-336.
[71]
Nijampurkar V N , Bhandari N , Vohra C P, et al. Radiometric chronology of Nehnar Glacier, Kashmir[J]. JGlaciol , 1982, 28: 91-105.
[72]
Nijampurkar V N, Amin B S, Kharkar D P, et al. Dating ground waters of ages younger than 1000-1500 years using natural silicon-32[J]. Nature, 1966, 210 (5035): 478-480.
[73]
Lal D. Some comments on applications of cosmogenic radionuclides for determining groundwater flow, with special reference to 32Si and 10Be[C/OL]. Paper presented at the SAHRA Recharge Workshop held at New Mexico Tech (Socorro). New-Mexico (U.S.A.): 2001[2005-10-05]. http:∥sahra.arizona.edu/events/workshops/20010322Recharge/pdf/lal_devendra.pdf.
[74]
刘存富,王佩仪,周炼,等. 河北山前平原地下水32Si年龄初探[J]. 水文地质工程地质,1999,2:1-9. Liu Cunfu, Wang Peiyi, Zhou Lian, et al. A preliminary study to the datiing of groundwater from Shanqian plain in Hebei Province using32Si method[J]. Hydrogeology and Engineering Geology, 1999, 2: 1-9(in Chinese).
[75]
刘存富,王佩仪,周炼. 应用天然测定32Si地下水年龄的新方法切伦科夫计数法[J]. 地质科技情报,1996,15(2):83-88.Liu Cunfu, Wang Peiyi, Zhou Lian. New method for dating ground water using natural32Si—Gerenkov`s counting method[J]. Geological Science and Technology Information, l996, 15(2): 83-88(in Chinese ).
[76]
刘存富,王佩仪,周炼,等. 地下水32Si年龄测定方法-液体闪烁计数法[J]. 水文地质工程地质,1997,6:5-9.Liu Cunfu, Wang Peiyi, Zhou Lian, et al. Dating of the groundwater by32Si—liquid scintillation counting method[J]. Hydrogeology and Engineering Geology, 1997, 6: 5-9 (in Chinese).
[77]
周炼,刘存富,王佩仪. 地下水32硅年龄的测定方法-液体闪烁计数法[J]. 岩矿测试,2000,19(2):97-100. Zhou Lian, Liu Cunfu, Wang Peiyi. Dating of the groundwater by32Si—liquid scintillation counting method[J]. Rock and Mineral Analysis, 2000, 19(2): 97-100(in Chinese ).
[78]
Morgenstern U, Cellermann R, Hebert D, et al.32Si in the limestone aquifers[J]. Chemical Geology, 1995, 120: 127-134.
[79]
Einloth S, Ekwurzel B, Eastoe C, et al. Progress on the Development of32Si as a Potential Tracer for Century-scale Recharge in Semi-arid Regions[C/OL][2005-10-05]. http:∥www.sahra.arizona.edu/events/meetings/2002annmeeting/posters/Einloth Sharon-Si32.pdf.
[80]
Einloth S, Ekwurzel B, Lal D, et al.32Si: A New Method for Estimating Semi-arid Vadose Zone Recharge[R/OL] [2005-10-05]. http:∥www. sahra.arizona.edu/publications/2001_ann_meeting/present_wed/TA2-2_Einloth_Sharon.pdf,
[81]
Frohich K, Frank T, Gellermann G, et al. Silicon-32 in different aquifer types and implications for groundwater dateing. [C]∥Proc. Int. Symp. Isotopic techniques in water resource development. Vienna: IAEA, 1987: 149-163.
[82]
Aertsens M, De Cannière P, Moors H. Modelling of silica diffusion experiments with 32Si in Boom Clay[J]. Journal of Contaminant Hydrology, 2003, 61: 117-129.
