高级检索
    王延亮, 侯伟, 侯占清, 熊绍礼. 略论吉林省大骨节病与地质环境的关系[J]. 中国地质, 2010, 37(3): 577-581.
    引用本文: 王延亮, 侯伟, 侯占清, 熊绍礼. 略论吉林省大骨节病与地质环境的关系[J]. 中国地质, 2010, 37(3): 577-581.
    WANG Yan-liang, HOU Wei, HOU Zhan-qing, XIONG Shao-li. The relationship between the Kaschin-Beck disease and the geological environment in Jilin Province[J]. GEOLOGY IN CHINA, 2010, 37(3): 577-581.
    Citation: WANG Yan-liang, HOU Wei, HOU Zhan-qing, XIONG Shao-li. The relationship between the Kaschin-Beck disease and the geological environment in Jilin Province[J]. GEOLOGY IN CHINA, 2010, 37(3): 577-581.

    略论吉林省大骨节病与地质环境的关系

    The relationship between the Kaschin-Beck disease and the geological environment in Jilin Province

    • 摘要: 提要:大骨节病流行于中山、低山和极低地区(低平原、山间谷地),元素迁移区和富集区,中偏酸性的还原环境和碱性-氧化环境。非病区则在元素流失区向元素富集区过渡的过渡带内,中性氧化还原环境。大骨节病是诸多地质环境因素综合影响的地方性疾病,但水文地球化学环境是最重要的因素。

       

      Abstract: Abstract:The Kaschin-beck disease is an epidemic disease widespread in such environments as middle-low mountains, low-lying lands (low plain and intermountain valley basin), migration and enrichment areas of elements, and intermediate-acid reducing and alkaline-oxidizing conditions. The non-disease area lies in the transitional zone from the depletion to the enrichment of elements in a neutral oxidization-reduction environment. The Kaschin-Beck disease is a disease affected by various geological environmental factors, in which hydrogeochemistry is the most important factor.

       

    /

    返回文章
    返回