Factors influencing the isotopically exchangeable phosphate in soils. Part II. The effect of base saturation with sodium and calcium in non-calcareous soils

9 pages, 5 tables, 10 references.

Saved in:
Bibliographic Details
Main Authors: Arambarri, Pablo de, Talibudeen, O.
Format: artículo biblioteca
Language:English
Published: Springer 1959-11
Online Access:http://hdl.handle.net/10261/77980
Tags: Add Tag
No Tags, Be the first to tag this record!
id dig-irnas-es-10261-77980
record_format koha
spelling dig-irnas-es-10261-779802016-02-17T19:11:15Z Factors influencing the isotopically exchangeable phosphate in soils. Part II. The effect of base saturation with sodium and calcium in non-calcareous soils Arambarri, Pablo de Talibudeen, O. 9 pages, 5 tables, 10 references. The effect of base saturation of non-calcareous soils with sodium and calcium on their total labile phosphate was studied in solutions of sodium and calcium chlorides of the same ionic strength (micro= 0.02). The total labile phosphate in 6 out of 7 soils was between 8 to 40 per cent higher in sodium saturated soils than in calcium-saturated soils. A much larger part of the total labile phosphate was found in solution in the sodium-saturated soils. The ratio of phosphate in solution in these soils to that in calcium-saturated soils varied from 3.4 to 8.1 with a mean value of about 5.5 as compared with a theoretical value of 4.1. A method is suggested for obtaining 'corrected' values for the abnormally high phosphate concentrations in solution from sodium-saturated soils. 'Corrected' values give smaller differences between the total labile phosphate in sodium and calcium forms of these soils. Rates of isotopic exchange of the more slowly exchanging forms of soil phosphate were measured at 25° and 35°C for the sodium- and calcium saturated forms of one Rothamsted soil. At 25°C these rates were four times higher in the sodium-saturated soil than in the calcium-saturated soil although the total labile phosphate in the two forms was the same. Increasing the temperature to 35°C doubled these rates of exchange in the sodium saturated soil but had no effect on the calcium-saturated soil. This suggests that the cation-exchangeable calcium is strongly linked to the slowly exchanging forms of phosphate in the soil. No differences were observed in the rates of isotopic exchange of phosphate in this soil after calcium saturation with either 0.01 molar or 1.0 molar calcium chloride. The precipitation of calcium phosphates during the calcium saturation procedure could not therefore be responsible for the observed differences between sodium- and calcium-saturated samples. Peer reviewed 2013-06-12T07:15:14Z 2013-06-12T07:15:14Z 1959-11 artículo http://purl.org/coar/resource_type/c_6501 Plant and Soil XI(4): 355-363 (1959) 0032-079X http://hdl.handle.net/10261/77980 10.1007/BF01371734 1573-5036 en http://dx.doi.org/10.1007/BF01371734 open Springer
institution IRNAS ES
collection DSpace
country España
countrycode ES
component Bibliográfico
access En linea
databasecode dig-irnas-es
tag biblioteca
region Europa del Sur
libraryname Biblioteca del IRNAS España
language English
description 9 pages, 5 tables, 10 references.
format artículo
author Arambarri, Pablo de
Talibudeen, O.
spellingShingle Arambarri, Pablo de
Talibudeen, O.
Factors influencing the isotopically exchangeable phosphate in soils. Part II. The effect of base saturation with sodium and calcium in non-calcareous soils
author_facet Arambarri, Pablo de
Talibudeen, O.
author_sort Arambarri, Pablo de
title Factors influencing the isotopically exchangeable phosphate in soils. Part II. The effect of base saturation with sodium and calcium in non-calcareous soils
title_short Factors influencing the isotopically exchangeable phosphate in soils. Part II. The effect of base saturation with sodium and calcium in non-calcareous soils
title_full Factors influencing the isotopically exchangeable phosphate in soils. Part II. The effect of base saturation with sodium and calcium in non-calcareous soils
title_fullStr Factors influencing the isotopically exchangeable phosphate in soils. Part II. The effect of base saturation with sodium and calcium in non-calcareous soils
title_full_unstemmed Factors influencing the isotopically exchangeable phosphate in soils. Part II. The effect of base saturation with sodium and calcium in non-calcareous soils
title_sort factors influencing the isotopically exchangeable phosphate in soils. part ii. the effect of base saturation with sodium and calcium in non-calcareous soils
publisher Springer
publishDate 1959-11
url http://hdl.handle.net/10261/77980
work_keys_str_mv AT arambarripablode factorsinfluencingtheisotopicallyexchangeablephosphateinsoilspartiitheeffectofbasesaturationwithsodiumandcalciuminnoncalcareoussoils
AT talibudeeno factorsinfluencingtheisotopicallyexchangeablephosphateinsoilspartiitheeffectofbasesaturationwithsodiumandcalciuminnoncalcareoussoils
_version_ 1777664613887770624