[1]Rea D K.The paleoclimatic record provided by eolian deposition in the deep sea:The geologic history of the wind[J].Reviews of Geophysics,1994,32:159-195. [2]李耀辉.近年来我国沙尘暴研究新进展[J].中国沙漠,2004,24(5):616-622. [3]韩永翔,张强,董光荣,等.沙尘暴的气候环境效应研究进展[J].中国沙漠,2006,26(2):307-311. [4]李栋梁,王涛,钟海玲,等.中国北方沙尘暴气候成因及未来趋势预测[J].中国沙漠,2004,24(3):376-379. [5]张小曳.亚洲粉尘的源区分布、释放、输送、沉降与黄土堆积[J].第四纪研究,2001,2(11):29-40. [6]Duce R A,Unni C K,Ray B J,et al.Long-range atmospheric transport of soil dust from Asia to the tropical North Pacific: Temporal variability[J].Science,1980,209:1522-1524. [7]赵凤生,石广玉.气溶胶气候效应的一维模式分析[J].大气科学,1994,18(增刊):902-909. [8]Martin J H,Fitzwater S E.Iron deficiency limits phytoplankton growth in the north-east pacific subarctic[J].Nature,1988,331:341-343. [9]Zhuang G,Yi Z,Duce R A.Link between iron and sulfur suggested by the detection of Fe(II)in remote marine aerosols[J].Nature,1992,355:537-539. [10]Jickells T D,An Z S,Andersen K K,et al.Global iron connections between desert,dust,ocean biogeochemistry,and climate[J].Science,2005,308:68-71. [11]Elderfield H.Carbonate Mysteries[J].Science,2002,296:1618-1620. [12]Monastersky R.A dusty way to break the ice age spell[J].Science News,1997,15:1-28. [13]IPCC.IPCC Second Assessment Report:Climate Change[M].Cambridge:Cambridge University Press,1995: 64. [14]张小曳,张光宇,朱光华,等.中国源区粉尘的元素示踪[J].中国科学:D辑,1996,26(5):424-430. [15]朱震达,吴正,刘恕,等.中国沙漠概论(修订版)[M].北京:科学出版社,1980:9-90. [16]彭红霞,李长安,杨桂芳,等.黄土中碳酸盐含量变化及其古气候记录——以兰州红咀寺剖面为例[J].地质科技情报,2003,22(1):53-55. [17]Jenny H.The Soil Resource [M].New York:Springer,1980:23-27. [18]郝永萍,方小敏,奚晓霞,等.青藏高原东北部及邻近地区土攘发育与气候定量模型的初步探讨[J].兰州大学学报:自然科学版,1995,31(2):165-170. [19]刘东生.黄土与环境[M].北京:科学出版社,1985:1-412. [20]文启忠.中国黄土地球化学[M].北京:科学出版社,1989:115-159. [21]Hao Q Z,Guo Z T.Spatial variations of magneticsusceptibility of Chinese loess for the last 600 kyr:Implication for monsoon evolution[J/OL].J Geophys Res,2005,110,B12101,doi:10.1029/2005JB003765. [22]Sun D H,Chen F H,Bloemendal J,et al.Seasonal variability of modern dust over the Loess Plateau of China[J/OL].J Geophys Res,2003,108(D21),4665,doi:10.1029/2003JD003382. [23]郭正堂,魏兰英,吕厚远,等.晚第四纪风尘物质成分的变化及其环境意义[J].第四纪研究,1999,19(1):41-48. [24]叶玮.中国西风区黄土常量元素地球化学行为与古环境[J].干旱区地理,2003,26(1):23-29. [25]张虎才.元素表生地球化学特征及理论基础[M].兰州:兰州大学出版社,1997:3-5. [26]王亚强,曹军骥,张小曳,等.中国粉尘源区表土碳酸盐含量与碳氧同位素组成[J].海洋地质与第四纪地质,2004,24(1):113-117. [27]曹军骥,王亚强,张小曳,等.大气中碳酸盐的碳同位素分析及其来源指示意义[J].科学通报,2004,49(17):1785-1788. [28]王宏,石广玉,Aoki T,等.2001年春季东亚-北太平洋地区沙尘气溶胶的辐射强迫[J].科学通报, 2004,49(19):1993-2000. [29]延昊, 矫海燕,毕宝贵,等.塔克拉玛干沙漠中心的沙尘气溶胶观测研究[J].中国沙漠,2006,26(3):389-393. [30]李玉霖,拓万全,崔建垣.兰州市沙尘和非沙尘天气沉降物的化学特性比较[J].中国沙漠,2006,26(4):648-651. [31]刘立超,王涛,周茅先,等.沙坡头地区沙尘气溶胶质量浓度的试验观测研究[J].中国沙漠,2005,25(3):337-341. [32]梅凡民,张小曳,鹿化煜,等.中国北方表土微团粒粒度分布及其对粉尘释放通量的影响[J].科学通报,2004,49(17):1776-1784. |