Stone research on the bench: where we are and where we are going.
Stone research on the bench: where we are and where we are going.
复制标题
板凳上的石头研究:我们现在在哪里,我们要去哪里。
DOI:
10.1089/089277902760261473
复制
发表时间:
2002
影响因子:
2.7
通讯作者:
Khan,SaeedR
中科院分区:
文献类型:
--
作者:
Khan,SaeedR
KIDNEY STONE FORMATION involves cellular and extracellular events. Extracellular events occur in renal tubular lumens and renal pelvises, while cellular events take place in the renal cells including cells of the renal epithelium and interstitium. In the middle part of the 20th century most of the basic research was concerned with extracellular events, primarily those special characteristics of the urine, which distinguished stone formers urine from non-stone-formers urine. It was suggested that urine from non-stone-forming individuals contained substances that inhibit crystallization. Urine with these inhibitory substances was considered “good” and urine without them,“evil.” 1 Pyrophosphate, citrate, magnesium, and an unidentified low molecular weight component were considered the main ingredients of good urine. It was also suggested that urine may contain substances that promote crystallization by inducing heterogeneous nucleation of crystals. In this regard, organic matrix of stones and a uromucoid called “Matrix Substance A” were studied in great detail. 2 It was well understood that human urine exists in a metastable supersaturated state. As a result, great emphasis was placed on understanding the solubility concepts and interactions between various factors responsible for maintaining supersaturation and influencing crystal nucleation, growth and aggregation. 3–5 Early researchers considered oxalate (Ox) to be a metabolic waste product that was excreted harmlessly. 6 Ox became harmful only after associating with calcium and forming calcium oxalate (CaOx) crystals and, even then, only when CaOx crystals could not be innocuously passed as crystalluria particles. It was calculated that passage through the nephron is fast, less than 3 min from one end of the nephron to the other, and that the growth of crystals was not fast enough for their retention based only on their size. It was concluded that crystal retention within the nephron through fixation was essential for stone formation. 7