Lecture-Notes on Theoretical Chemistry (Paperback)


This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1893 Excerpt: ...of the oxides which are isomorphous, are then added together. Thus: SiO, = 36.02 H-00 = 0.6103, Al, O, = 7.53-h 102 = 0.0738, Pe, O, = 22.18 4-160 = 0.1380, CaO = 31.80-4-56 = 0.5678, MgO = 1.95-i-40 = 0.0487. Adding respectively the values for Al, O, and for Fe, O, and the values for CaO and for MgO, there results: SiO, = 0.6103 = 3, (Al, O, .Fe, O, ) = 0.2118 = 1, (CaO.MgO) = 0.6165 = 3; which result is the same as that previously obtained. The formula of the mineral as derived from these data can be expressed as: 3(CaMgO), (Al, Fe.O, ),3SiO, or as: (CaMg), (Al, Fe, )Si, O1, . In accordance with the custom of mineralogists, who prefer to represent the formulae of such minerals even more concisely, the letter R can be used to denote metallic radicals, and Roman numerals placed above the same, can be made to indicate the valence of the radicals: The above formula would thus be written: II VI IV R, (R, )Si, Oi, a shorter, and an equally correct expression of the composition of this mineral. A formula of this kind can easily be changed to a formula n in the old dualistic system, by converting R into RO and VI (R, ) into R, O, . 'It would then read: 3RO, R, O, Si, O, . Comparing now the quantities of oxygen in combination with the several bases and with the silicon, it will be seen that they bear to one another the relation 3:3:6; that is, as 1: 1: 2. This ratio, in this instance 1: 1: 2, is termed the oxygen ratio, and it will be noticed that it is the same as the ratio of the total valence, the so-called atomic ratio, of each radical in the formula: For, II X 3 = 6; VI X 1 = 6; IV X 3 = 12. and 6: 6: 12, is the same ratio as 1: 1: 2. If it be required to calculate the mineralogical formula of a silicate from its percentage composition, the first step to be taken wil

R532

Or split into 4x interest-free payments of 25% on orders over R50
Learn more

Discovery Miles5320
Free Delivery
Delivery AdviceOut of stock

Toggle WishListAdd to wish list
Review this Item

Product Description

This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1893 Excerpt: ...of the oxides which are isomorphous, are then added together. Thus: SiO, = 36.02 H-00 = 0.6103, Al, O, = 7.53-h 102 = 0.0738, Pe, O, = 22.18 4-160 = 0.1380, CaO = 31.80-4-56 = 0.5678, MgO = 1.95-i-40 = 0.0487. Adding respectively the values for Al, O, and for Fe, O, and the values for CaO and for MgO, there results: SiO, = 0.6103 = 3, (Al, O, .Fe, O, ) = 0.2118 = 1, (CaO.MgO) = 0.6165 = 3; which result is the same as that previously obtained. The formula of the mineral as derived from these data can be expressed as: 3(CaMgO), (Al, Fe.O, ),3SiO, or as: (CaMg), (Al, Fe, )Si, O1, . In accordance with the custom of mineralogists, who prefer to represent the formulae of such minerals even more concisely, the letter R can be used to denote metallic radicals, and Roman numerals placed above the same, can be made to indicate the valence of the radicals: The above formula would thus be written: II VI IV R, (R, )Si, Oi, a shorter, and an equally correct expression of the composition of this mineral. A formula of this kind can easily be changed to a formula n in the old dualistic system, by converting R into RO and VI (R, ) into R, O, . 'It would then read: 3RO, R, O, Si, O, . Comparing now the quantities of oxygen in combination with the several bases and with the silicon, it will be seen that they bear to one another the relation 3:3:6; that is, as 1: 1: 2. This ratio, in this instance 1: 1: 2, is termed the oxygen ratio, and it will be noticed that it is the same as the ratio of the total valence, the so-called atomic ratio, of each radical in the formula: For, II X 3 = 6; VI X 1 = 6; IV X 3 = 12. and 6: 6: 12, is the same ratio as 1: 1: 2. If it be required to calculate the mineralogical formula of a silicate from its percentage composition, the first step to be taken wil

Customer Reviews

No reviews or ratings yet - be the first to create one!

Product Details

General

Imprint

Rarebooksclub.com

Country of origin

United States

Release date

May 2012

Availability

Supplier out of stock. If you add this item to your wish list we will let you know when it becomes available.

First published

2010

Authors

Dimensions

246 x 189 x 3mm (L x W x T)

Format

Paperback - Trade

Pages

56

ISBN-13

978-1-152-36875-0

Barcode

9781152368750

Categories

LSN

1-152-36875-3



Trending On Loot