R Institution | 9 Mar 1837
My dear Sir
I have been engaged the last three or four day[s] in analyzing your clays1. (You know analyses are very tedious & time consuming things) and now send you the results[.]
The pit clay in its moist state has a specific gravity of 2.07. This you required to know though I do not see what use it can be of to you. It contains a trace of carbonate of lime but it also contains little calcareous concretions like small pebbles which would render a specimen carelessly taken very uncertain in its composition[.] In its moist state as sent to me a hundred parts contain the follow‑ing proportions very nearly
The Medway clay in its dark coloured & moist state had a Specific Gravity of 1.46 but this of course would vary as the quantity of water varied. 100 parts gave
I have put down all the iron as per oxide because it is the best state in which to estimate it but in the clay whilst dark coloured a portion of it is in the con‑dition of Sulphuret (the greater portion being even then per oxide) and the presence of this sulphuret causes the dark colour & also the evolution of Sulphuretted hydrogen upon the affusion of acids - a little protoxide may also be present[.]
The gases you speak of as existing in the clay do not exist in it really but are produced from the wood & organic matter - the carbonate of lime & the Sulphuret of iron &c &c by the action of heat[.]
Ever Dear Sir | Very Truly Yours | M. Faraday
Coll. Pasley | &c &c &c
Address: Coll. Pasley | &c &c &c | Chatham
PASLEY, Charles William (1838): Observations on Limes, calcareous cements, mortars, stuccos and concrete, and on puzzolanas natural and artificial, London.
Please cite as “Faraday0979,” in Ɛpsilon: The Michael Faraday Collection accessed on 1 May 2024, https://epsilon.ac.uk/view/faraday/letters/Faraday0979