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庐山是长江流域中部的名山,位于鄱阳湖西北面,其地理位置约为北纬29度/35分及东经116度。庐山最高峯的海拔略高于1,500米,它虽不是一座高山,但为避暑胜地,并且是不同领域的自然科学工作者所爱好的科学研究场所。朱显谟曾对庐山土壤作过研究,他着重报导了庐山主要土类的分布和形态。本文报告庐山主要土类的理化性状及其他特征的研究结果。所采取的土样皆分布于自庐山次高峯大月山(海拔约1,450米)经含鄱口,下至山之东南麓白鹿洞一線,其中仅自大月山不远所选的一个剖面在此線之外。本文特别着重于山上土壤与山麓低丘土壤差异的
Mount Lushan, a famous mountain in the middle of the Yangtze River valley, is located northwest of Poyang Lake. Its geographical location is about 29 degrees north latitude and 35 minutes longitude and 116 degrees east longitude. The elevation of Lushan Peak is slightly higher than 1,500 meters above sea level. Although it is not a mountain, it is a summer resort and a scientific research site favored by natural science workers in different fields. Zhu Xianmo had done research on the soil of Lushan, he focused on the distribution of Lushan major soil types and morphology. This paper reports the physical and chemical properties and other characteristics of the major soil types in Lushan. The soil samples taken were all from the Lushan sub-peak Damanshan (about 1,450 meters above sea level) passing through the Han Pokou and down to the southeast foot of Bailu-dong of the mountain, of which a section Beyond this line. This article focuses particularly on differences in soil between hills and foothills