Hostname: page-component-586b7cd67f-t7czq Total loading time: 0 Render date: 2024-11-25T04:07:24.785Z Has data issue: false hasContentIssue false
  • English
  • Français

Studies of a Scottish drift soil

Published online by Cambridge University Press:  27 March 2009

James Hendrick  and
George Newlands
James Hendrick
Affiliation:
(Soil Research Department, North of Scotland College of Agriculture, Aberdeen.)
George Newlands
Affiliation:
(Soil Research Department, North of Scotland College of Agriculture, Aberdeen.)
Get access Rights & Permissions [Opens in a new window]

Extract

1. An examination is made of some aspects of the replacement or exchange of bases by ammonium chloride solution, in a soil about which considerable information had been acquired regarding its physical, chemical, and mineralogical constitution, namely, the soil of Craibstone Experiment Farm, Aberdeen. Certain data in this connection are given.

2. The “course of replacement” of calcium by ammonia, by successive applications of equal amounts of a normal solution of ammonium chloride is examined, according to the method of Gedroiz. Comparison is made between the results got for the Craibstone soil and those for a tshernoziem soil examined by Gedroiz. By means of graphs the agreement between the two soils as to the “course of replacement” is shown, and a distinction made between easily extractable calcium, and that more slowly removed in solution. The “course of replacement” of potassium and magnesium in the Craibstone soil is also examined.

3. The presence of silicon, aluminium, iron and manganese is also noted in the extracts.

4. The soil is also examined for “Total Exchangeable Bases” by extraction with normal ammonium chloride, according to the method of Hissink, with minor modifications.

5. Exchangeable aluminium, iron, calcium, magnesium, manganese, potassium and sodium were found and in addition silicon was present in the extracts.

6. The question of the presence of silicon, aluminium, iron and manganese in measurable amounts in extracts from acid soils is discussed.

7. The relative proportions of exchangeable divalent and monovalent bases found were as follows. Calcium 85·02 per cent., magnesium 8·11 per cent., potassium 2·18 per cent., sodium 4·68 per cent. These results are in general agreement with those found for acid soils.

Type
Research Article
Information
The Journal of Agricultural Science , Volume 16 , Issue 4 , October 1926 , pp. 584 - 595
Copyright
Copyright © Cambridge University Press 1926

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

1Gedroiz, K. K. (1914). Colloidal Chemistry as related to Soil Science, Part II, Section 2. Zhur. Opit. Agron. 15, 181–205. (Trans. Dr S. A. Waksman, New Jersey Exp. Sta.)Google Scholar
2Gedroiz, K. K. (1914). Colloidal Chemistry as related to Soil Science, Part II, Section 2. Zhur. Opit. Agron. 15, 181–205. Table I.Google Scholar
3Gedroiz, K. K. (1918). Contribution to the method of Determining the Zeolitic Bases in the Soil. Zhur. Opit. Agron. 19, 226–244. (Trans. Dr S. A. Waksman.)Google Scholar
4Gedroiz, K. K. (1916). The Absorbing Capacity of the Soil and Soil Zeolitic bases. Zhur. Opit. Agron. 17, 484 (Table III). (Trans. Dr S. A. Waksman.)Google Scholar
5Gedroiz, K. K. (1916). The Absorbing Capacity of the Soil and Soil Zeolitic bases. Zhur. Opit. Agron. 17, p. 489.Google Scholar
6Gedroiz, K. K. (1916). The Absorbing Capacity of the Soil and Soil Zeolitic bases. Zhur. Opit. Agron. 17, p. 476.Google Scholar
7Gedroiz, K. K. (1916). The Absorbing Capacity of the Soil and Soil Zeolitic bases. Zhur. Opit. Agron. 17, p. 481 (Table II).Google Scholar
8Hendrick, J. and Newlands, G. (1923). The value of mineralogical examination in determining Soil Types. Journ. Agric. Sci. 13, Part I, pp. 1–16.CrossRefGoogle Scholar
9Hendrick, J. and Ogg, W. G. (1916). Studies of a Scottish Drift Soil. Part I. Journ. Agric. Sci. 7, Part IV, pp. 458–469.CrossRefGoogle Scholar
10Hendrick, J. and Ogg, W. G. (1916). Studies of a Scottish Drift Soil. Part I. Journ. Agric. Sci. 7, p. 461.CrossRefGoogle Scholar
11Hissink, D. J. (1923). Method for Estimating Absorbed bases in Soils. Soil Science, 15, 271.CrossRefGoogle Scholar
12Kelly, W. P. and Brown, S. M. (1924). Replaceable Bases in Soils. Agric. Exp. Sta. California Univ. Tech. Paper No. 15, p. 5.Google Scholar
13Kelly, W. P. and Brown, S. M. (1924). Replaceable Bases in Soils. Agric. Exp. Sta. California Univ. Tech. Paper p. 6.Google Scholar
14Kelly, W. P. and Brown, S. M. (1924). Replaceable Bases in Soils. Agric. Exp. Sta. California Univ. Tech. Paper p. 20.Google Scholar
15Ogg, W. G. and Hendrick, J. (1920). Studies of a Scottish Drift Soil. Parts II and III. Journ. Agric. Sci. 10, Part 3, pp. 53–77.Google Scholar
16Smith, A. M. (1925). The Exchangeable Bases in Some Scottish Soils. Journ. Agric. Sci. 15, Part 4, p. 472.CrossRefGoogle Scholar
17Smith, A. M. (1925). The Exchangeable Bases in Some Scottish Soils. Journ. Agric. Sci. 15, p. 471.CrossRefGoogle Scholar