The Amount of Free Lime and the Composition of the Soluble Phosphates in Basic Slag

1909 ◽  
Vol 3 (2) ◽  
pp. 161-170 ◽  
Author(s):  
C. G. T. Morison

Basic Slag owes its value as a source of phosphoric acid to the fact that it is essentially basic in its character, and can be used on land where an acid manure of the character of superphosphate is not to be recommended.As no figures were available on the subject it seemed interesting to determine how much of the lime which it contains existed in the free uncombined condition. It has been stated that in some cases this is as much as 20%.With a view to this determination four samples of freshly ground slag were obtained direct from the makers through the kindness of the Lawes Chemical Manure Company.

1915 ◽  
Vol 35 ◽  
pp. 195-202 ◽  
Author(s):  
A. Lauder ◽  
T. W. Fagan

The various factors which are supposed to influence the composition of milk have already been the subject of numerous investigations. The general result of these has been to show that within very wide limits the composition of milk is very little affected by the nature of the food supplied. As regards the mineral constituents the results of some of the investigations are rather conflicting, and while there is a general consensus of opinion that the composition and amount of the mineral constituents are independent of the food-supply, certain investigators claim to have been able to increase both the calcium and phosphoric acid in the milk by slight amounts.


1920 ◽  
Vol 3 (3) ◽  
pp. 286-288
Author(s):  
C S Lykes
Keyword(s):  

2018 ◽  
Vol 149 ◽  
pp. 01075 ◽  
Author(s):  
A. Bouregba ◽  
A. Diouri ◽  
B. Elghattas ◽  
A. Boukhari ◽  
T. Guedira

It has been found that the addition of certain components, despite their low concentration in raw mix, may accelerate and enhance the reactivity of the cement raw mix. The utilization of mineralizers to facilitate and quicken the process of clinkerization backpedals numerous years, the concept of using such mineralizers to burn normal raw mixes at a much lower temperature with the end goal of decreasing the fuel necessities of the furnace and to enhance the cement proprieties has become to be seriously considered over the most recent couple of years. The subject of this paper is to investigate the impact of calcium fluoride as mineralizer on addition during the clinkerization process of industrial raw mixtures and its effect on chemical, mineralogical, and mechanical properties of CPA Moroccan cement. Five different raw meals were utilized and were burned with 2% of calcium fluoride. The resulting clinker was analyzed by X-ray diffraction (XRD) and fluorescence spectroscopy to determine the chemical phases of the obtained clinker, and the mechanical properties of resulting CPA cement were determined. The results show that the addition of 2% of CaF2 to the clinker raw meal induced a decrease in the burning temperature and free lime, while improving the clinker phase formation and the mechanical properties of obtained cement.


In 1894 the author contributed to the ‘Journal of the Chemical Society’ (vol. 65, ‘ Trans.,’ March, 1894) a paper 011 “ The Determination of Available Mineral Plant Food in Soils,” in which the use of a 1 per cent, solution of citric acid was proposed as a means of approximately differentiating by means of chemical analysis between the total and the probably available phosphoric acid and potash in soils. The reasons leading up to the tentative adoption of this solution, together with a summary of previous literature on the subject, are given in the original paper, and it need, therefore, now only be said that the method was the result of an attem pt to imitate, in the solvent used, the acidity of root-sap, based on a preliminary examination of the root acidity of 100 specimens of flowering plants representing some 20 natural orders. In order to test the proposed method it was applied to 22 samples of soil drawn from the various plots in Hoos Field, Rothamsted, on which barley under very various manurial conditions had been continuously grown for over forty years. The samples were placed at the author’s disposal by the kindness of Sir John Lawes and Sir Henry Gilbert. The results of this investigation, which are fully set forth in the paper referred to, were of sufficient interest to lead to the undertaking of a similar but much more extended examination of the soils of the Rothamsted wheat plots in Broadbalk Field.


1845 ◽  
Vol 16 (1) ◽  
pp. 53-59
Author(s):  
John Davy

The condition of the alkali in the blood—of that portion on which its alkaline reaction depends—has been the subject of much speculation, and of many experiments. Enderling is one of the latest inquirers who has given it his attention. After having made an analysis of the ashes of the blood, he has come to the conclusion, that the alkali in it is in combination with phosphoric acid, the former predominating in the form of the tribasic phosphate of soda.


1880 ◽  
Vol 30 (200-205) ◽  
pp. 278-286 ◽  

Among the results of a large investigation on which I have for many years been engaged in regard of the chemistry of the brain, I had been led to conclude that the so-called “ protagon” of Oscar Liebreich is not a definite chemical body, but is a variable mixture of several bodies. This conclusion of mine (which agrees with opinions expressed on the same subject by Strecker, Diaconow, and HoppeSeyler) was published by me in 1874, and endeavours to controvert it have since then been made, on several occasions, by Dr. Arthur Gamgee. Last summer, he brought before the Royal Society his contentions for the chemical individuality of “protagon”; and it fortunately was in my power shortly afterwards to publish evidence, which, I believe, those who will take the trouble to follow it will find quite unanswerable, that Dr. Gamgee’s contentions were mistaken.§ Part of my evidence to that effect consisted in showing by quantitative analyses that Dr. Gamgee’s so-called “ protagon” contains 0·7 per cent, of potassium; secondly, that in connexion with trifling differences in the extraction process, the proportion of potassium in different specimens of “protagon” can be made to range from a trace to 1·6 per cent.; thirdly, that with the variable quantities of potassium the quantities of phosphorus and other ingredients will also vary. In the last published number, No. 200, p. 111, of the “Proceedings of the Royal Society,” I find that Dr. Gamgee has recently brought the question again under notice of the Society, and that, in doing so, he especially rests his case upon the following statement made by his colleague, Professor Roscoe, on the subject of some examinations, which, at Dr. Gamgee’s request, he had made for him: see “ Proceedings,” vol. xxx, p. 113:—“I have examined spectroscopically for potash a sample of protagon furnished me by Dr. Gamgee, and labelled ‘Protagon, twice recrystallised, Blankenhom.’ I could not detect any potash by the spectroscope in the incinerated mass from 0·1 grm. of substance. With the carbonised mass obtained from 1·0 grm. of substance I obtained the potasssium line ( α ) very faintly, and from comparative experiments with a dilute solution of a potassium salt I estimate the quantity of potash in 1 grm. of the substance Lot to exceed 1/20 mgrm. The carbonised residue of 1 grm. of protagon was carefully oxidised with pure nitric acid, when a small quantity of fused metaphosphoric acid remained after ignition. The residue weighed 0·0278 grm., corresponding to 1·08 per cent, of phosphorus.— (Signed) H. E. Roscoe.”


1929 ◽  
Vol 19 (3) ◽  
pp. 586-588
Author(s):  
A. D. Hall

The last issue of this Journal (p. 132) contains a paper by Dr R. A. Fisher on the effect of Silica upon the growth of Barley at Rothamsted, which begins by stating that his data “show conclusively that the view previously rejected that the silicate acts by making available to the plant the actual reserves of soil phosphates must be regarded as strongly established.” Twice elsewhere Dr Fisher states that this erroneous conclusion of previous investigators is due to the fact that they had considered only the proportion of phosphoric acid in the ash and had overlooked the increase in the total phosphoric acid in the crop. As Mr Morison and I were the previous investigators in question I turned to our twenty-three-year-old paper with some curiosity to ascertain the grounds for this magisterial dismissal of our conclusions, for my remembrance of the subject did not tally with the opinion Dr Fisher attributes to us. Still less do I agree now that I have re-examined our original paper.


1864 ◽  
Vol 13 ◽  
pp. 520-531

The constitution, properties, and derivatives of the so-called conjugated sulphurous and sulphuric acids have been made the subject of numerous searches, and have led, in the hands of Gerhardt and others, to very interesting results. I have examined at different times several members of the methylsulphuric, phenylsulphurous, nitrophenvlsulphous and other series, but have lately turned my attention to the analogous compounds of the phosphoric series. Some remarkable substances have been thus made, their constitution seeming to have a direct bearing upon the important question of the atomicity and equivalency of certain of the metallic elements. Several substances might have served as starting-points for these new inquiries. A curious compound, phenylphosphoric acid, C 6 H 5 H 2 PO 4 , was prepared; but its instability, and the oxidation to which it and its salts are liable, rendered it unsuited for the present purpose. I intend to describe in the present paper but one series of salts, formed from Pelouze’s ethylphosphoric acid, C 2 H 5 H 2 PO 4 . This compound, containing two atoms of easily replaceable hydrogen, appeared admirably adapted for the purpose in view. It is readily prepared by digesting (for 48 hours) finely crushed glacial phosphoric acid with alcohol of 90 percent.:— C 2 H 5 H } O + H PO 3 = C 2 H 3 H H } PO 4 .


1920 ◽  
Vol 3 (4) ◽  
pp. 585-586
Author(s):  
C B Williams ◽  
B L Hartwell ◽  
H D Haskins ◽  
C G Hopkins ◽  
J A Bizzell
Keyword(s):  

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