Petrographic and geochemic evaluation of equine enteroliths

Citation
Dm. Hassel et al., Petrographic and geochemic evaluation of equine enteroliths, AM J VET RE, 62(3), 2001, pp. 350-358
Citations number
28
Categorie Soggetti
Veterinary Medicine/Animal Health
Journal title
AMERICAN JOURNAL OF VETERINARY RESEARCH
ISSN journal
00029645 → ACNP
Volume
62
Issue
3
Year of publication
2001
Pages
350 - 358
Database
ISI
SICI code
0002-9645(200103)62:3<350:PAGEOE>2.0.ZU;2-Y
Abstract
Objective-To characterize the texture, mineralogic features, and chemical f eatures of enteroliths obtained from horses. Sample Population-Enteroliths from 13 horses with colic. Procedure-Enteroliths were harvested from 13 horses that underwent ventral midline celiotomy for treatment of colic or necropsy because of colonic obs truction and rupture caused by enteroliths. Dietary and environmental histo ry were determined via questionnaires or evaluation of medical records. In 7 horses that underwent surgical treatment for enterolithiasis, samples of colonic contents were obtained via an enterotomy in the pelvic flexure. Col onic concentrations of magnesium (Mg), phosphorus (P), sulfur (S), sodium ( Na), calcium (Ca), and potassium (K) were determined. Enteroliths were anal yzed via electron microprobe analysis and X-ray diffraction. Results-Enteroliths varied widely regarding degree of porosity, presence an d distribution of radiating texture. and composition and size of the centra l nidus. A distinct concentric banding was identifiable in all enteroliths. Struvite was the predominant component of all enteroliths, although Mg viv ianite was identified in 5 enteroliths, and there were variable quantities of Na, S, K, and Ca in the struvite within enteroliths. Despite an abundanc e of Ca in colonic fluids, Mg-phosphate minerals were preferentially formed , compared with Ca-phosphates (apatite), in equine enteroliths. Conclusions and Clinical Relevance-Enteroliths comprise 2 major Mg phosphat es: struvite and Mg vivianite. There is wide variability in macrotexture an d ionic concentrations between and within enteroliths.