Hostname: page-component-586b7cd67f-dsjbd Total loading time: 0 Render date: 2024-11-26T04:02:32.220Z Has data issue: false hasContentIssue false

A simple method for the determination of the pH values of turbid soil and other solutions

Published online by Cambridge University Press:  27 March 2009

C. H. Gadd
Affiliation:
(Mycologist, Tea Research Institute of Ceylon.)

Extract

In the course of investigations into the cause of an obscure pathological condition of the tea bush, it became necessary to make pH determinations of certain soils. Electrometric apparatus and a suitable centrifuge for clearing the solutions were not available. Considerable difficulty was experienced in making the determinations with accuracy by indicator methods owing to two causes. First, the turbidity of the soil solutions made comparison with standard buffer solutions somewhat difficult; secondly, the colours developed in the soil and buffer solutions with some indicators were different in hue, as distinct from shade or tint. This rendered exact matching quite impossible. The latter difficulties also arose when the drop ratio method was used instead of standard buffer solutions. The errors resulting from these causes were believed to be unduly large, and it was felt that greater accuracy would be attained if these difficulties could be overcome.

Type
Research Article
Copyright
Copyright © Cambridge University Press 1928

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

(1)Atkins, W. R. G. (1925). “The hydrogen-ion concentration of plant cells.” Notes from the Bot. School, Trinity College, Dublin, 3, 178190.Google Scholar
(2)Clark, W. M. (1925). The determination of hydrogen-ions, Baltimore.Google Scholar