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茶叶科学 ›› 2006, Vol. 26 ›› Issue (2): 87-90.doi: 10.13305/j.cnki.jts.2006.02.002

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我国古红土与茶叶生长

陆景冈1, 吴建军1, 赵东2, 唐根年3   

  1. 1. 浙江大学环境与资源学院,浙江 杭州 310029;
    2.浙江大学茶叶研究所,浙江 杭州 310029;
    3. 浙江工业大学经贸学院,浙江 杭州 310014
  • 收稿日期:2005-10-26 修回日期:2006-02-27 出版日期:2006-06-25 发布日期:2019-09-10
  • 作者简介:陆景冈(1928- ),男,江苏南京人,教授,主要从事地质与茶学的教学和科研工作。

Red paleosols and Tea Plant Growth in China

LU Jing-gang1, WU Jian-jun1, ZHAO Dong2, TANG Gen-nian3   

  1. 1. College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310029, China;
    2. Tea Research Institute, Zhejiang University, Hangzhou 310029, China;
    3. Department of Business Administration, Zhejiang University of Technology, Hangzhou 310014, China
  • Received:2005-10-26 Revised:2006-02-27 Online:2006-06-25 Published:2019-09-10

摘要: 本文总结了全国网纹红土分布与长江以北大部茶树分布恰相符合;又分析了脱离于红壤带之外的山东日照茶区、西藏察隅茶区,其土壤都有古红土的影响,说明了是古红土促进了茶树生长。虽然古红土和现代红壤的关系,至今在科学上还未完全解决,但从实际出发,研究茶园土壤,古红土的影响不容忽视。

关键词: 古红土, 全国茶叶分布, 红壤带, 脱硅富铝化作用

Abstract: This paper tallied up that the distribution of plinthitic red paleosol is just coincide with the tea in the area north of Yantze River(Fig.1).Moreover, there are two tea areas outside of the red earth zone on the distributional map (Rizhao area in Shangdong Province. And Chayu area in Tibet)。It can be recognized that both of them had been influenced by the red paleosol on the soil property. All of these showed that the red paleosol could promote the tea plant growth.Therefore the influences of the red paleosol should not be negnected on the study of tea garden soil.

Key words: red paleosol, chinese tea plant distribution, red earth zone, desilisification-allitization

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