Please use this identifier to cite or link to this item:
Chromium Distribution in the Latosols of the Hawaiian Islands
|Title:||Chromium Distribution in the Latosols of the Hawaiian Islands|
Sherman, G. Donald
show 1 moreOxisols
|Date Issued:||Feb 1958|
|Publisher:||Hawaii Agricultural Experiment Station, University of Hawaii|
|Citation:||Nakamura M, Sherman GD. 1958. Chromium distribution in the latosols of the Hawaiian Islands. Honolulu (HI): Hawaii Agricultural Experiment Station, University of Hawaii. 12 p. (Technical Bulletin; 37)|
|Abstract:||The Hawaiian Islands were formed from basaltic lavas, some of which have high concentrations of pyroxene and olivine. Since chromium is associated with the foregoing minerals, it is reasonable to assume that the element is present in the soils of Hawaii. The present study was designed to determine the presence and the dislribution of the element in the various great soil groups formed through the process of laterizarion. Other objectives were to determine the correlation, if any, between chromium concentration and the intensity of weathering in the soils and the influence of the parent material on the accumulation of the element. This study will attempt to show that both these factors play important roles in the concentration of chromium in the Hawaiian soils which were analyzed.|
|Appears in Collections:||
Technical Bulletin, 1943 - 1980|
Please email firstname.lastname@example.org if you need this content in ADA-compliant format.
Items in ScholarSpace are protected by copyright, with all rights reserved, unless otherwise indicated.