中国地质
中國地質
중국지질
CHINESE GEOLOGY
2009年
5期
1154-1162
,共9页
中国七大古都%环境地球化学%丰度对比特征%历时-元素含量回归分析
中國七大古都%環境地毬化學%豐度對比特徵%歷時-元素含量迴歸分析
중국칠대고도%배경지구화학%봉도대비특정%력시-원소함량회귀분석
China's seven ancient capitals%environmental geochemistry%abundance contrast features%regression analysis of duration-elements
以全国水系沉积物地球化学调查成果为基础,讨论中国七大古都安阳、西安、洛阳、开封、南京、杭州、北京的环境地球化学背景特征,结果表明,与中国水系沉积物元素含量均值相比,七大古都所在地相对富集镁、钙、硼、锫、银、钴、钡、钠、锶和磷,以人体必需营养元素为主;同时相对贫化镉、钼、锑、铅、钨、铋、砷、锰、铌和汞等,以人体有害元素为主.根据土壤地球化学特征,欧洲的主要国都可分为波罗的海型和地中海型,具有不同的元素分布模式.在中国古都延续时间与元素偶比值之间可建立回归方程Y=0.206X+376,X=(CaO×Fe_2O_3×V×Co×10~6)/(SiO_2×Pb×Hg×Cd);在欧洲国都与元素偶比值之间也可建立类似的回归方程.充分说明首都的选址还受到地球化学环境的制约.
以全國水繫沉積物地毬化學調查成果為基礎,討論中國七大古都安暘、西安、洛暘、開封、南京、杭州、北京的環境地毬化學揹景特徵,結果錶明,與中國水繫沉積物元素含量均值相比,七大古都所在地相對富集鎂、鈣、硼、锫、銀、鈷、鋇、鈉、鍶和燐,以人體必需營養元素為主;同時相對貧化鎘、鉬、銻、鉛、鎢、鉍、砷、錳、鈮和汞等,以人體有害元素為主.根據土壤地毬化學特徵,歐洲的主要國都可分為波囉的海型和地中海型,具有不同的元素分佈模式.在中國古都延續時間與元素偶比值之間可建立迴歸方程Y=0.206X+376,X=(CaO×Fe_2O_3×V×Co×10~6)/(SiO_2×Pb×Hg×Cd);在歐洲國都與元素偶比值之間也可建立類似的迴歸方程.充分說明首都的選阯還受到地毬化學環境的製約.
이전국수계침적물지구화학조사성과위기출,토론중국칠대고도안양、서안、락양、개봉、남경、항주、북경적배경지구화학배경특정,결과표명,여중국수계침적물원소함량균치상비,칠대고도소재지상대부집미、개、붕、부、은、고、패、납、송화린,이인체필수영양원소위주;동시상대빈화력、목、제、연、오、필、신、맹、니화홍등,이인체유해원소위주.근거토양지구화학특정,구주적주요국도가분위파라적해형화지중해형,구유불동적원소분포모식.재중국고도연속시간여원소우비치지간가건립회귀방정Y=0.206X+376,X=(CaO×Fe_2O_3×V×Co×10~6)/(SiO_2×Pb×Hg×Cd);재구주국도여원소우비치지간야가건립유사적회귀방정.충분설명수도적선지환수도지구화학배경적제약.
According to data from geochemical stream sediment survey, this paper deals with the environmental geochemical background characteristics of China's seven ancient capitals, which include Anyang, Xi'an, Luoyang, Kaifeng, Nanjing, Hangzhou and Beijing. The results show that, compared with element contents of stream sediments in China, the body-oriented essential nutrients cal cium, boron, zirconium, silver, cobalt, barium, sodium, strontium and phosphorus are relatively high in areas of the seven ancient capitals. At the same time, these ancient capital areas are relatively depleted in cadmium, molybdenum, antimony, lead, tungsten, bismuth, arsenic, manganese, niobium and mercury, which are mainly harmful elements. In accordance with the soil geochemical characteristics, capitals of major European countries can be divided into the Baltic type and the Mediterranean type, which have different element distribution patterns. According to the relationship between the duration of the ancient capital and the ratio of elements, regression equations can be respectively established: Y_1 = 0.206X +376, X_1=(CaO×Fe_2O_3×V×Co×10~6)/(SiO_2×Pb×Hg×Cd) for China, and Y_2=395.61gX_2-115.5, X_2= (CaO×MgO×Fe_2O_3×Mn×Co×Cd)/(SiO_2×Sr) for Europe, suggesting that the site selection of a capital was restricted by the geochemical environment.