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A Ruiz de Aguiar

Publications and source records attributed to A Ruiz de Aguiar.

6 recordsLinked to original sources

[Primary lithiasis of the choledochus: etiologic factors and structural characteristics].

OBJECTIVE: To study clinical and morphological characteristics of primary gall stones in the common bile duct in order to establish a differential diagnosis with migrating stones. DESIGN: To analyze a number of clinical parameters (age, parity, evolution, number of stones and diameter), qualitative parameters (sex, obesity, cholecystitis, cholangitis, liver disease or previous biliary surgery) and statistic evaluation. To show composition of stones throw stereomicroscope, electronic microscope and dispersion analysis by X-Ray. PATIENTS: We studied 56 patients who were diagnosed and operated of choledocholithiasis. RESULTS: 21 cases (37.5%) were considered as primary stones (group "a") and 35 (62.5%) were considered as migrating stones (group "b"). We have found significant statistical differences in relationship with the age of patients (p < 0.05) and diameter of stones (p < 0.01). They were both greater in primary stones, while the rest of parameters were not significant. Brown pigment stones dominate in primary stones followed by calcium palmitate and cholesterol stones. We identified bacteria or their traces (38.1%), foreign bodies (19.04%), carbonate of calcium (38.1%) and phosphate of calcium (9.5%). CONCLUSIONS: They are clinical and morphological characteristics which may differentiate between primary and migrating common duct stones. The high incidence of germs or foreign bodies found in the core layer of stones show their importance in the formation of brown pigment.

Aged↗

[The composition and structure of cholesterol biliary calculi].

The order and composition of the various elements that are present in the cholesterol stones has been analyzed and a useful model that should help in the study of already formed stones is proposed and therefore a better understanding of the lithogenesis and the physiopathological conditions in which stones develop. The existing components are described from the core up to the crust, case emphasizing the heterogeneity of the core, the calcium palmitate around it and the cholesterol disposition. The various forms of presentation of calcium carbonate are defined as well as the different types of ooliths.

Cholelithiasis↗

Calcium carbonate in cholesterol gallstones.

CaCO3 has been studied in twelve gallstones in which cholesterol predominated. Different polymorphs of CaCO3, as well as carbonate-apatite, were characterised by X-ray diffraction, polarised light microscopy and scanning electron microscopy. Crystals and rhombohedral aggregates of calcite, aggregates of small crystals and tabular crystals of vaterite and fibrous radial aggregates in the form of ooliths were found. In microscopic studies on sections of the stones, CaCO3 was localised mainly in the periphery in the form of layers or bands associated with calcium bilirubinate which was deposited in close relation to it. The phenomena contributing to the precipitation of CaCO3 are discussed, as is the importance of the latter in resistance to the pharmacologic treatment of gallstone disease.

Adult↗