sunshinesunshine文章编号: 1008-181X (2000) 04-0330-03棕红壤区土壤中的锌及其生物利用途径胡学玉 1, 2,李学垣1,谢振翅2( 1:华中农业大学资源环境与农业化学系,湖北武汉 430070 ;2:湖北省农科院土壤肥料研究所,湖北武汉430064 )摘要: 从改善人体锌营养状况的角度,阐述了棕红壤区土壤中的锌含量及其影响锌有效性的多种因素。指出棕红壤区土壤锌资源较为丰富。研究和培育富锌作物品种,提高作物可食部位含锌量,是缓解人类锌营养不良的有效途径之一。关键词:棕红壤;锌;生物利用中图分类号: S153.6 =1 文献标识码: A Zinc in Brown Red Soil and Its Bio-utilization HU Xue-yu1, 2, LI Xue-yuan1, XIE Zhen-chi2 ( 1: Department of Resources Environment and Agro-chemistry, Huazhong Agricultural University, Wuhan 43007 ,China; 2: Soil and Fertilizer Institute, Hubei Academy of Agricultural Sciences, Wuhan 430064, China ) Abstract: This paper covered the zinc content and the factors affecting zinc availability in brown red soil from the angle of improving human Zn-nutrition, pointing out that the soil was rich in zinc element. It was a realistic and sustainable solution to the problem of human Zn-nutrition malnutrition by breeding of Zn-dense plant gene-types with better capacity to acquire zinc from soils. Key words: brown red soil; zinc; bio-utilization1 棕红壤丘陵区土壤中的锌含量湖北省的棕红壤主要分布于鄂东南海拨500 m 以下的低山、丘陵和岗地,处于黄壤与红壤间的过渡带,是鄂东南低山丘陵区典型的地带性土壤。根据已有资料,棕红壤全锌量在46~83 g/g之间,有效锌量在0.5~1.44 g/g之间,平均为0.86 g/g 。影响土壤锌含量的因素主要有下面几种。1.1成土母质土壤锌含量在很大程度上决定于成土母质的锌含量。鄂东南低山丘陵区棕红壤的成土母质主要包括花岗岩、片麻岩、砂岩、页岩、石灰岩及第四纪红色粘土等,其中以石灰岩发育的棕红壤锌含量较高,砂岩发育的棕红壤锌含量较低[1] 。1.2 成土过程成土过程是成土母质中化学元素重新组合的过程,它改变了母质中微量元素的初始含量,改变了它们的结合特性...