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The Precipitation of Sparingly Soluble Metal Salts Factors Affecting Crystal Form and Anisometry (II)

โœ Scribed by Dr. A. Packter; P. Chauhan; D. F. Saunders


Publisher
John Wiley and Sons
Year
1969
Tongue
English
Weight
524 KB
Volume
4
Category
Article
ISSN
0232-1300

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โœฆ Synopsis


This paper describes studies on the factors that determine the crystal form and anisometry of sparingly-soluble metal acetates, benzoates, oximates and 'oxinates' precipitated from aqueous solution : previous studies on metal phenylarsonate precipitates are also examined.

Generally, needle-shaped and fibrous crystals are formed by met'al organic salts and chelates with the larger divalent metal atoms (radius > 1.3 d) and cations (radius > 0.8 A) of cadmium, lead, copper; also by nickel glyoxime.

The anisometry ( p ) of the precipitates studied is enhanced by precipitation at low metal salt concentration (c) -supersaturation, s = 1 to 10 -, a t reduced p H and from aqueous -organic solvent solutions containing 10 to 50 per cent polar organic solvents. p varies with c according to the relation, p = p , c -~.

The factors that lead to p~eferent~ial growth onto one crystal face and hence to crystal anisometry are discussed.

Es werden die Faktoren behandelt, die die Kristallform und Anisometrie schwach loslicher Metallacetate, -benzoate, -oximate und ,,-oxinate" aus wasserigen Losungen bestimmen. Fruhere Untersuchungen an Metallphenylarsonat-Niederschlagen werden ebenfalls betrachtet.

Im allgemeinen bilden sich nadelformige und faserige Kristalle von metallorganischen Salzen und Chelaten mit grofieren bivalenten Metallatomen (Radius > 1.3 A) und Kationen (Radius > 0.8 A) von Cadmium, Blei und Kupfer; ebenfalls von Nickelglyoxim. Die Anisometrie ( p ) der untersuchten Niederschlage wird erhoht durch FBllung bei niedriger Metallsalzkonzentration (c) -UbersBttigung s = 1 bis 10 -, bei verringertem PH und aus Losungen mit wasserigen organischen Losungsmitteln, die 10 bis 15% polare organische Flussigkeiten enthalten. p iindert sich mit c entsprechend der Beziehung p = p1 c -~. Die Faktoren, die zum bevorzugten Wachsen einer Kristallflache und damit zur Kristallanisomet,rie fiihren, werden besproc,hen.


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