地质科技情报
地質科技情報
지질과기정보
GEOLOGICAL SCIENCE AND TECHNOLOGY INFORMATION
2009年
6期
107-113
,共7页
毛绪美%王焰新%Oleg V.Chudaev
毛緒美%王燄新%Oleg V.Chudaev
모서미%왕염신%Oleg V.Chudaev
水化学%富CO_2矿泉%中国东北%俄罗斯远东
水化學%富CO_2礦泉%中國東北%俄囉斯遠東
수화학%부CO_2광천%중국동북%아라사원동
hydrogeochemistry%CO_2-rich mineral spring%Northeast China%the Far East Russia
中国东北与俄罗斯远东富CO_2矿泉是宝贵的饮用、医用矿水资源.五大连池、长白山天池、俄罗斯远东Primorye地区各泉水水化学特征对比显示,中国东北五大连池与俄罗斯远东Primorye地区出露泉水为低温、微酸、HCO_3型、富含Si、Fe、Sr和CO_2气体的综合优质饮用矿泉水;长白山天池出露泉水为高温、中性-微碱、HCO_3型、富含Si和CO_2气体的优质热矿泉水.五大连池和俄罗斯远东富CO_2冷矿泉与长白山天池富CO_2热矿泉具有相似而不同的形成过程,CO_2气体对水化学的形成起了决定性的作用,广泛发育的花岗岩提供了富CO_2热泉的物质来源,断层破碎带增加了CO_2气体-地下水-花岗岩之间的反应程度,温度仅对可溶性Si有影响.
中國東北與俄囉斯遠東富CO_2礦泉是寶貴的飲用、醫用礦水資源.五大連池、長白山天池、俄囉斯遠東Primorye地區各泉水水化學特徵對比顯示,中國東北五大連池與俄囉斯遠東Primorye地區齣露泉水為低溫、微痠、HCO_3型、富含Si、Fe、Sr和CO_2氣體的綜閤優質飲用礦泉水;長白山天池齣露泉水為高溫、中性-微堿、HCO_3型、富含Si和CO_2氣體的優質熱礦泉水.五大連池和俄囉斯遠東富CO_2冷礦泉與長白山天池富CO_2熱礦泉具有相似而不同的形成過程,CO_2氣體對水化學的形成起瞭決定性的作用,廣汎髮育的花崗巖提供瞭富CO_2熱泉的物質來源,斷層破碎帶增加瞭CO_2氣體-地下水-花崗巖之間的反應程度,溫度僅對可溶性Si有影響.
중국동북여아라사원동부CO_2광천시보귀적음용、의용광수자원.오대련지、장백산천지、아라사원동Primorye지구각천수수화학특정대비현시,중국동북오대련지여아라사원동Primorye지구출로천수위저온、미산、HCO_3형、부함Si、Fe、Sr화CO_2기체적종합우질음용광천수;장백산천지출로천수위고온、중성-미감、HCO_3형、부함Si화CO_2기체적우질열광천수.오대련지화아라사원동부CO_2랭광천여장백산천지부CO_2열광천구유상사이불동적형성과정,CO_2기체대수화학적형성기료결정성적작용,엄범발육적화강암제공료부CO_2열천적물질래원,단층파쇄대증가료CO_2기체-지하수-화강암지간적반응정도,온도부대가용성Si유영향.
CO_2-rich mineral springs , valuable resources for drinking and medical purpose are found in Northeast China and the Far East Russia. Comparison of chemical characteristics of springs water shows that high quality drinking water can be found in Wudalianchi and Primorye mineral springs with the characteristics of low temperature, slightly acidic, HCO_3 type, rich in Si, Fe, Sr and CO_2 gas, different from that of Changbaishan Tianchi springs with higher temperature, neutral to slight-alkali, HCO_3 type, rich in Si and CO_2 gas. CO_2-rich cold mineral springs of Wudalianchi and the Far East Russia have similar but different formation process to those of Changbaishan Tianchi. CO_2 gas plays a decisive role in the formation of water chemistry, while wide-spread granite provides chemical materials, and the fractured zone of the fault improves the interaction between CO_2 gas-groundwater-granite. However, the temperature only influences the soluble Si.