物探与化探
物探與化探
물탐여화탐
GEOPHYSICAL AND GEOCHEMICAL EXPLORATION
2014年
2期
325-330
,共6页
严明书%龚媛媛%杨乐超%周皎%张茂忠%鲍丽然
嚴明書%龔媛媛%楊樂超%週皎%張茂忠%鮑麗然
엄명서%공원원%양악초%주교%장무충%포려연
重庆%富硒土%经济意义%土壤地球化学
重慶%富硒土%經濟意義%土壤地毬化學
중경%부서토%경제의의%토양지구화학
Chongqing%Se-rich topsoil%economic significance%soil geochemistry
通过重庆表层土壤网格化及岩土剖面取样测量,对重庆表层土壤Se的地球化学特征及丰缺进行研究。结果表明,重庆浅层土壤Se含量范围为(0.005~5.790)×10-6,背景值为0.197×10-6。土壤Se含量分布受地层、母岩岩性、土壤类型、土壤层位及土壤对Se富集特性的控制。高Se土壤主要分布在三叠系、二叠系、志留系、奥陶系及寒武系的石灰土中。以土壤Se含量(0.400~3.000)×10-6为富硒土标准,已调查发现重庆分布富硒土3684 km2,在綦江南部-万盛-南川一带,在主城区周边天俯、花溪、三汇等小面积分布,推测在武隆-酉阳-秀山及城口-巫山一带存在大面积富硒土,重庆可能拥有上万平方千米富硒土。富硒土区pH环境、有机质含量有利于农产品安全,已发现北碚天府富硒土区谷物类及十字花科类农产品为富硒无公害或富硒绿色农产品。重庆富硒土具良好经济意义。
通過重慶錶層土壤網格化及巖土剖麵取樣測量,對重慶錶層土壤Se的地毬化學特徵及豐缺進行研究。結果錶明,重慶淺層土壤Se含量範圍為(0.005~5.790)×10-6,揹景值為0.197×10-6。土壤Se含量分佈受地層、母巖巖性、土壤類型、土壤層位及土壤對Se富集特性的控製。高Se土壤主要分佈在三疊繫、二疊繫、誌留繫、奧陶繫及寒武繫的石灰土中。以土壤Se含量(0.400~3.000)×10-6為富硒土標準,已調查髮現重慶分佈富硒土3684 km2,在綦江南部-萬盛-南川一帶,在主城區週邊天俯、花溪、三彙等小麵積分佈,推測在武隆-酉暘-秀山及城口-巫山一帶存在大麵積富硒土,重慶可能擁有上萬平方韆米富硒土。富硒土區pH環境、有機質含量有利于農產品安全,已髮現北碚天府富硒土區穀物類及十字花科類農產品為富硒無公害或富硒綠色農產品。重慶富硒土具良好經濟意義。
통과중경표층토양망격화급암토부면취양측량,대중경표층토양Se적지구화학특정급봉결진행연구。결과표명,중경천층토양Se함량범위위(0.005~5.790)×10-6,배경치위0.197×10-6。토양Se함량분포수지층、모암암성、토양류형、토양층위급토양대Se부집특성적공제。고Se토양주요분포재삼첩계、이첩계、지류계、오도계급한무계적석회토중。이토양Se함량(0.400~3.000)×10-6위부서토표준,이조사발현중경분포부서토3684 km2,재기강남부-만성-남천일대,재주성구주변천부、화계、삼회등소면적분포,추측재무륭-유양-수산급성구-무산일대존재대면적부서토,중경가능옹유상만평방천미부서토。부서토구pH배경、유궤질함량유리우농산품안전,이발현북배천부부서토구곡물류급십자화과류농산품위부서무공해혹부서록색농산품。중경부서토구량호경제의의。
Geochemical characteristics and content of selenium (Se) in the topsoil of Chonqing City were investigated on the basis of measuring the topsoil in Chongqing obtained from gridding and section sampling. The content of Se in the topsoils of Chonqing City is (0.005~5.790)×10-6 , and the background level is 0.197×10-6 . The distribution of Se is controlled by the strata, the lithology of the mother rock, the types of the soil, the horizon of the soil and the controlling capability of the soil for enriching the Se. The Se-rich soil is distributed mainly in the Triassic, Permian, Devonian, Silurian, Ordovician and Cambrian calcareous soil. According to the standard that the Se-rich soil should have the Se content of (0.4~3.0)×10-6 , a total area of 3 684 km2 of Se-rich soil was discovered, which is distributed mainly in the south of Qiqiang-Wansheng-Nanchuan district, with a small amount distributed in places near the Chongqing main city, like Tianfu, Huaxi and Sanhui. It is inferred that there also exists over 10 000 km2 of Se-rich soil in Wulong-Youyang-Xius-han and Chengkou-Wushan areas. The Se-rich soil is favorable for enriching the Se in the primary product, because of the pH and the organic matter in the Se-rich environment. It has been proved that the primary products are green primary products in Beibei Se-rich soil area. The Se-rich soil in Chongqing has good economic significance.