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地理科学 2013

连云港藤花落遗址土壤粒度及重金属累积特征

, PP. 349-355

周华,廖富强,徐明星,周生路,吴绍华

Keywords: 藤花落遗址,龙山文化,重金属累积,粒度,江苏省

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Abstract:

对江苏北部连云港龙山文化时期藤花落遗址城市生活区(L1)剖面和农业生产区(L2)剖面土壤重金属累积及土壤粒度特征分析发现,龙山文化时期人类活动已经出现明显土壤重金属累积,但影响仅局限人类生活区,农业生产区无累积现象;Cu、Pb和Zn累积最为明显,富集指数分别达到1.91、1.35和1.29,该遗址文明已进入铜石并用时代。同时分析土壤粒度发现,遗址文明存在期间曾发生过大规模或长时间水患事件,破坏农业生产条件,最终导致整个文明走向衰落。重金属累积及土壤粒度的综合分析,揭示史前文明演变的过程及其与自然环境变迁的规律。

References

[1]	Walkington H.Soil science applications in archaeological contexts:A review of key challenges[J].Earth-Science Reviews,2010,103(3-4):122-134.
[2]	Wilson C A,Davidson D A,Cresser M S.Multi-element soil analysis:an assessment of its potential as an aid to archaeologicalinterpretation[J]. 2008,(35):412-424.
[3]	Hong S,Candelone J,Patterson C C.History of Ancient CopperSmelting Pollution During Roman and Medieval Times Recordedin Greenland Ice[J].Science,1996,272:246-249.
[4]	Hong S,Candelone J,Patterson C C.Greenland Ice Evidence ofHemispheric Lead Pollution Two Millennia Ago by Greek andRoman Civilizations[J].Science,1994,265:1841-1843.
[5]	Vesely J.The history of metal pollution recorded in the sedimentsof Bohemian Forest lakes:Since the Bronze Age to thepresent[J].Silva Gabreta,2000,4:147-166.
[6]	Luo X,Yu S,Zhu Y,et al.Trace metal contamination in urbansoils of China[J/OL]. doi:10.1016/j.scitotenv.2011.04.020
[7]	Maisto G,Alfani A,Baldantoni D, et al. Trace metals in the soiland in Quercus ilex L.leaves at anthropic and remote sites ofthe Campania Region of Italy[J].Geoderma,2004,122(2-4):269-279.
[8]	张丽萍,王小云,张赫斯.沙盖黄土丘陵坡地土壤理化特性随地形变化规律研究[J].地理科学,2011,31(02):78~183.
[9]	吴文祥,刘东生.4 000 a B.P.前后东亚季风变迁与中原周围地区新石器文化的衰落[J].第四纪研究,2004,24(3):278~284.
[10]	李兰,朱诚,姜逢清,等.连云港藤花落遗址消亡成因研究[J].科学通报,2008,(53):139~152.
[11]	涤烦子.连云港藤花落遗址考古新发现[J].江苏地方志,2004,(3):32.
[12]	周润垦,李洪波,张浩林,等.2003~2004 年连云港藤花落遗址发掘收获[J].东南文化,2005,(3):15~19.
[13]	Wu S,Zhou S,Li X,et al.Heavy-metal accumulation trends inYixing,China:an area of rapid economic development[J].EnvironEarth Sci,2010,61:79-86.
[14]	Zhang H,Shan B.Historical records of heavy metal accumulationin sediments and the relationship with agricultural intensificationin the Yangtze-Huaihe region,China[J].Science of the TotalEnvironment,2008,339:113-120.
[15]	Kabata-Pendias A, Mukherjee A. Trace elements from soil tohuman[M]. Berlin: Springer, 2007: 267-276.
[16]	廖启林,刘聪,许艳,等. 江苏省土壤元素地球化学基准值[J].中国地质,2010,38(5): 1363~1378.
[17]	徐利斌,孙立广,张居中,等.公元前2500 年: 中国进入铜石并用时代的汞记录[J].第四纪研究,2008,28(6):1070~1080.
[18]	路迪民.论中国铜石并用时代和青铜器时代的分期[J].西安建筑科技大学学报,1999,18(1):47~51.
[19]	陈栋栋,彭淑贞,张伟,等.山东全新世典型气候事件的区域响应及其对海岱文明发展的影响[J]. 地理科学进展,2011,18(7):846~852.
[20]	张冉,刘晓东.中全新世暖期与未来气候变暖情景下东亚夏季降水变化相似型分析[J].地理科学,2009, 29(5): 679~683.
[21]	王军,高红山,潘保田,等.早全新世沙沟河古洪水沉积及其对气候变化的响应[J].地理科学,2010,30(6):943~949.
[22]	吴绍华,周生路,杨得志,等.宜兴市近郊土壤重金属来源与空间分布研究[J].科学通报,2008,53(增刊I):162~170.
[23]	Zhang G,Zhu C,Wang J,et al.Environmental archaeology onLongshan Culture (45 00-4 000 a B.P.) at Yuhuicun Site inBengbu, Anhui Province[J].J.Geogr.Sci.,2010,20(3):455-468.
[24]	舒强, 赵志军, 陈晔, 等.江苏兴化DS浅孔沉积物地球化学元素与粒度所揭示的古环境意[J].地理科学,2009, 29(6):923~928.
[25]	王心源,吴立,张广胜,等.安徽巢湖全新世湖泊沉积物磁化率与粒度组合的变化特征及其环境意义[J].地理科学,2008,28(4):548~553.
[26]	Nyder W S,Cook M J,Nasset E S,et al.Report of the task groupon reference man. International Commission on RadiologicalProtection No 23[M].Oxford:Pergamon Press,1975.
[27]	Alexandrovskaya E I,Alexandrovskiy A L.History of the culturallayer in Moscow and accumulation of anthropogenic substancesin it[J].Catena,2000,41(1-3):249-259.
[28]	Leyden B W, Brenner M, Dahlin B H. Cultural and ClimaticHistory of Coba′, a Lowland Maya City in Quintana Roo, Mexico[J].Quaternary Research,1998,49:111-122.
[29]	Oonk S,Slomp C P,Huisman D J.Geochemistryas an Aid in ArchaeologicalProspection and Site Interpretation:Current Issuesand Research Directions[J].Archaeol Prospect 2009,16:35-51.
[30]	Wei B,Yang L.A review of heavy metal contaminations in urbansoils,urban road dusts and agricultural soils from China[J]. MicrochemicalJournal,2010,94:99-107.
[31]	廖富强.苏北沿海滩涂土壤性质和景观格局时空变化研究[D].南京:南京大学博士论文,2008.
[32]	吴绍华,周生路,张红富,等.经济发展梯度影响下的江苏农用地土壤重金属含量分布格局[J].地理科学,2008,28(3):412~418.
[33]	Hu X,Wang C,Zou L.Characteristics of heavy metals and Pb isotopicsignatures in sediment cores collected from typical urbanshallow lakes in Nanjing,China[J].Journal of EnvironmentalManagement. 2011,92:742-748.
[34]	李月芳,姚檀栋,王宁练,等.帕米尔东部慕士塔格冰芯Sb 浓度变化记录揭示的近50a 来中亚区域人类活动[J].冰川冻土,2008,30(6):359~364.
[35]	韩桂红,塔西甫拉提·特依拜,买买提·沙吾提,等.渭-库绿洲地下水对土壤盐渍化和其逆向演替过程的影响[J].地理科学,2012,32(3): 362~367.
[36]	Summers J,Wade T,Engle V.Normalization of metal concentrationsin estuarine sediments from the Gulf of Mexico[J].Estuaries,1996,19:581-594.

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