机构地区: 浙江工业大学经贸管理学院
出 处: 《茶叶科学》 2001年第2期85-89,共5页
摘 要: 名茶产地的成土母质主要有石英砂岩、花岗岩、酸性凝灰岩与片麻岩等 ,它们在浙江被两条地质深大断裂分隔为三区 ,而各区的母质又各有特点。从新构造运动看 ,名茶多分布在强烈上升的山地区和沿海的升沉过渡丘陵区。从局部环境看 ,名茶产地附近多有湖、海等巨大水体。各类成土母质对茶品质的影响可用地球化学性质来解释 ,有关的元素有Si、K、Fe、Al、Ca、Mg、Mn等。文中还从已发现的名茶产地地质学规律出发 。 Parent materials of the soils in famous_tea producing area are mainly quartz sandstone, granite, acidic tuff and gueiss. Zhejiang province and its neighbour area can be divided by two big deep reaching faults into three regions , and there are different character for each region. In the view of geotectonic movement most of the famous_tea producing field is located on the uplifted mountain area with a higher altitude or on the lower hilly area by the side of subsided plain or sea, which belong to the transitional area from uplift to subside. Besides, most famous_tea producing field is often near by a large body of water, such as lake, sea, etc. The influences of parent material on tea quality can be explained by rock geochemistry. Those elements such as Si, Al, Fe, Ca, Mg, Mn, etc in the rock and soil are associated. In the view of geopedologic law the author discussed the development strategy of famous_tea production.