NOTE ON THE USE OF FLOODING SOLUTIONS IN THE DETERMINATION OF METALLIC EXCHANGEABLE CATIONS, UTILIZING A BECKMAN DU FLAME SPECTROPHOTOMETER

1962 ◽  
Vol 42 (2) ◽  
pp. 317-318 ◽  
Author(s):  
J. A. Carson ◽  
A. L. Mathieu ◽  
M. D. Scheelar
Keyword(s):  

not available

2015 ◽  
Vol 29 (1) ◽  
pp. 31-37 ◽  
Author(s):  
Ewa A. Czyż ◽  
Anthony R. Dexter

Abstract A method for the experimental determination of the amount of clay dispersed from soil into water is described. The method was evaluated using soil samples from agricultural fields in 18 locations in Poland. Soil particle size distributions, contents of organic matter and exchangeable cations were measured by standard methods. Sub-samples were placed in distilled water and were subjected to four different energy inputs obtained by different numbers of inversions (end-over-end movements). The amounts of clay that dispersed into suspension were measured by light scattering (turbidimetry). An empirical equation was developed that provided an approximate fit to the experimental data for turbidity as a function of number of inversions. It is suggested that extrapolation of the fitted equation to zero inversions enables the amount of spontaneously-dispersed clay to be estimated. This method introduces the possibility of replacing the existing subjective, qualitative method of determining spontaneously-dispersed clay with a quantitative, objective method. Even though the dispersed clay is measured under saturated conditions, soil samples retain a ‘memory’ of the water contents at which they have been stored.


2012 ◽  
Vol 45 (2) ◽  
pp. 135-142 ◽  
Author(s):  
Ye-Jin Lee ◽  
Hong-Bae Yun ◽  
Rog-Young Kim ◽  
Jong-Sik Lee ◽  
Yo-Sung Song ◽  
...  

1991 ◽  
Vol 71 (2) ◽  
pp. 155-163 ◽  
Author(s):  
Pat E. Rasmussen ◽  
Sherry L. Schiff ◽  
H. Wayne Nesbitt

To investigate pH-controlled chemical reactions associated with the neutral salt measurement of exchangeable cations in acid soils, and to estimate the potential error caused by such reactions, a series of experiments was performed which modify an established BaCl2 extraction method. Results showed that dissolution of amorphous silica, aluminum hydroxides and organic material occurs during neutral salt extraction, contributing cations to solution which are indistinguishable from exchangeable cations. As a result overestimates of exchangeable Al and Ca occur, but the error is not significant (> 10%) except in certain Ae horizons which are low in total CEC and high in exchangeable acidity. The 2-h BaCl2 method is recommended over the 4-hour NaCl method to minimize interference from weathering reactions. Key words: Cation exchange, exchangeable acidity, Al, H, acid forest soils, weathering


2000 ◽  
Vol 56 (5) ◽  
pp. 766-772 ◽  
Author(s):  
Florence Porcher ◽  
Mohamed Souhassou ◽  
Heinz Graafsma ◽  
Anna Puig-Molina ◽  
Yves Dusausoy ◽  
...  

An accurate knowledge of zeolite structure is required for understanding their selective sorption capacities and their catalytic properties. In particular, the positions of the exchangeable cations and their interactions with the framework are essential. The present study deals with the accurate crystal structure determination of a fully exchanged and fully dehydrated CaA zeolite (Ca48Al96Si96O384, Fm\bar 3c, a = 24.47 Å) using single-crystal high-resolution synchrotron X-ray diffraction [(sin θ/λ)max = 1.4 Å−1]. It is shown that cation exchange severely distorts the skeleton, especially around the O2 atom. The high-resolution synchrotron data reveal that this latter O atom is disordered and lies out of the mirror plane it occupies in other A-type zeolites. This feature is related to that observed for Ca2+ cations.


Agronomie ◽  
1997 ◽  
Vol 17 (1) ◽  
pp. 9-16 ◽  
Author(s):  
H. Ciesielski ◽  
T. Sterckeman ◽  
M. Santerne ◽  
J. P. Willery

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