Further evidence linking urolithiasis and blood coagulation: urinary prothrombin fragment 1 is present in stone matrix

The fact that organic material is always present and distributed throughout each renal calculus suggests that it may play a role in stone formation. The organic matrix of calcium oxalate (CaOx) crystals freshly generated in urine in vitro contains urinary prothrombin fragment 1 (UPTF1) as the principal protein. In this initial study, matrix was extracted from 12 renal calculi and evaluated for the presence of UPTF1 using Western blotting. UPTF1 was present in all eight stones whose principal component was CaOx, and in one of two stones which consisted mainly of calcium phosphate (CaP). UPTF1 was absent from the two struvite calculi examined. The relationship between CaP and UPTF1 was explored further. Matrix harvested from CaP crystals freshly generated in urine in vitro was also shown to contain UPTF1 as its principal component. Our inability to detect UPTF1 in one mixed CaOx/CaP stone may be related to our methods of matrix retrieval, while its absence from two struvite stones argues against it being present in the other stones merely as a consequence of passive inclusion. This absence may be related to the alkaline environment typical of struvite stone growth. The finding that UPTF1 is present in some renal stones provides the first direct evidence that links blood coagulation proteins with urolithiasis.     

Genomic screen for QTLs underlying alcohol consumption in the P and NP rat lines

PURPOSE: We examined the effects of human urine on the adhesion of calcium oxalate monohydrate (COM) crystals to Madin-Darby canine kidney (MDCK) cells in vitro. METHODS: Quantitative assay of COM crystal adhesion to MDCK cells: MDCK cells were exposed to COM crystal suspension for 5 minutes. Various urine samples were added in the COM crystal suspension. The adherent COM crystals on the MDCK cells were dissolved by 5 N hydrochloric acid. Calcium concentration of the solution was measured by atomic absorption analysis to quantify the volume of adherent COM crystals. This assay was applied for the experiments as follows. (1) Effect of human urine on COM crystal adhesion. (2) To investigate whether human urine inhibited COM crystal adhesion by acting on the crystal surface or on the cell surface. (3) Isolation of the substance from human urine that inhibits COM crystal adhesion. (4) Comparison of the inhibitory activities of the urine between from stone formers and healthy controls. RESULTS AND CONCLUSION: (1) Human urine had a strong inhibitory effect on COM crystal adhesion to MDCK cells. (2) The capacity of human urine to inhibit adhesion of COM crystals to MDCK cells was shown to be mediated by their ability to act on the crystal surface. (3) We isolated a macromolecular fraction (MW 60,000) that had strong capacity to inhibit cellular adhesion of COM crystals through ion exchange and gel filtration chromatography. (4) Nine urine samples from stone formers demonstrated extreme low inhibitory activities, which supposed us that the inhibitory capacity of the urine against crystal adhesion might be one of the risk factors in kidney stone formation.     

Biochemical characterization of a delta12 acyl-lipid desaturase after overexpression of the enzyme in Escherichia coli

OBJECTIVE: To study the variability in urine composition with respect to factors of importance for the calcium salt crystallization process and to test the reliability of using one or several urine samples in the clinical evaluation. PATIENTS AND METHODS: Twelve patients collected 16-hour daytime and 8-hour night urine samples during 4 days of the same week. The urine was analysed for calcium, oxalate, phosphate, magnesium, citrate and pH, and the ion activity products of CaOx [AP(CaOx) index] and CaP were calculated. The risk of CaOx crystallization, as well as the inhibition of CaOx crystal growth and aggregation, were assessed. RESULTS: There was a good correlation between estimates of the AP(CaOx) index in the different samples, as well as between the AP(CaOx) index and the direct assessment of the risk of CaOx crystallization in the night and daytime urine samples. There was, however, a pronounced intra-individual variation of all variables and parameters. With the assumption that an abnormality would appear in at least one of the four samples, we found that in more than 80% of the cases, two 24-hour (16 + 8 h) urine samples were sufficient to establish whether the patient had a normal or an abnormal urine composition. CONCLUSION: Urine samples collected during two 24-, 16- or 8-hour periods appear to be useful for detecting biochemical abnormalities considered of importance for CaOx stone formation.     

Adhesion and endocytosis of calcium oxalate crystals on renal tubular cells

The present investigation was designed to study interactions between Madin-Darby canine kidney (MDCK) cells and calcium oxalate monohydrate (COM) crystals and to clarify the significance of these crystal-cell interactions in stone pathogenesis. MDCK cells cultured in the presence of COM crystals showed a time-dependent uptake of crystals; this was specific for COM crystals. In the dynamic model system designed to study these phenomena under more physiological conditions, COM crystals adhered to the cell surface and were subsequently internalized. In this endocytotic process, the microvilli of the cell appeared to play an important role. The observation by scanning electron microscopy of complexes consisting of aggregated COM crystals and cell debris led us to speculate that adhesion and endocytosis of crystals might provide the calculus nidus for aggregation and retention of crystals in the renal tubule. Furthermore, glycosaminoglycans and the macromolecular fraction of human urine were shown to have the ability to inhibit the cellular uptake of crystals. Evidence that similar processes may also occur in vivo was obtained using an experimental stone model in rats. Our experiments revealed that most of the COM crystals adhered to the tubular cells and some crystals were endocytosed by the cell. Thus, these crystal-cell interactions might be one of the earliest processes in the formation of kidney stones. Further elucidation of the mechanism and the regulatory factors involved in this process may provide new insight into stone pathogenesis.     

Histone deacetylase. A key enzyme for the binding of regulatory proteins to chromatin

Stone and urine composition were analysed in 75 men and 40 women with recurrent calcium oxalate stone disease (group R) and in 48 men and 19 women who had formed only one calcium-oxalate-containing stone (group S). Patients who had developed stones with a large fraction of calcium phosphate were significantly more frequent in group R than in group S. There was furthermore a higher excretion of calcium and higher calcium oxalate supersaturation levels in patients with stones containing more than 25% calcium phosphate. It was concluded from these observations that the calcium phosphate content of renal stones might be a useful factor in predicting the future course of the disease.     

Renal metabolic changes relating to calculogenesis in an experimental model of calcium containing renal stone formation in rabbits

In histochemical studies it was shown that sulfated acid glycosaminoglycans (AGAGS) were produced and secreted into the tubular lumen in renal papilla, but not in the renal cortex of muddy stone forming kidney. There was no secretion of sulfated AGAGS in renal papilla histochemically during hydronephrosis before stone formation. On autoradiographic study with the use of 45Ca and 35S for labeling of sulfated AGAGS, we found that 45Ca accumulated in renal papilla of muddy stone forming kidney, but not in the other. 35S apparently accumulated into muddy stones. Measurement of calcium content of the renal papilla and cortex proved the results of autoradiographic studies, and measurement of uronic acid in the urine showed increased secretion of AGAGS in the urine from muddy stone forming kidney. From these results it was proposed that the sulfate AGAGS secreted in the urine could bind calcium crystals to each other amd make crystals aggregate massively.     

Accurate determination of chemical composition of urinary calculi by spiral computerized tomography

PURPOSE: Choice of efficacious clinical management of symptomatic renal calculi can be facilitated by ascertaining the precise chemical composition of the calculus. Spiral computerized tomography (CT) is becoming a frequently used radiographic examination to establish the diagnosis and severity of calculus disease. Our objective for this study was to determine the precision of spiral CT in identifying the chemical composition of 6 different types of urinary calculi with region of interest measurements using spiral CT. MATERIALS AND METHODS: A total of 102 chemically pure stones were separated into 6 groups. The stones along with phantoms containing butter (fat) and jello (water) were mounted vertically in the scanner gantry. Then 1 mm. thickness scanning was performed with a high speed scanner at the 2 energy levels of 80 and 120 kV. The determination of the chemical composition was performed using the absolute CT value measured at 120 kV. and the dual kilovolt CT values measured at 80 and 120 kV. Hounsfield unit at 80 kV.-Hounsfield unit at 120 kV.). RESULTS: The absolute CT value measured at 120 kV. was able to identify precisely the chemical composition of uric acid, struvite and calcium oxalate stones. It was imprecise in differentiating calcium oxalate from brushite stone and struvite from cystine stone. However, dual kilovolt CT value was able to differentiate these latter stones with statistical significance (p < 0.03). Uric acid stones were easily differentiated from all other stones using the absolute CT value. CONCLUSIONS: This study demonstrates that the chemical composition of urinary calculi can be accurately determined by CT scanning in an in vitro setting.     

Urinary calcium oxalate saturation in healthy infants and children

PURPOSE: A number of factors influence the development of renal calculi, the most essential of which is the supersaturation of urine with lithogenic substances. Calcium oxalate stones occur most frequently in adult and pediatric patients with urolithiasis. Therefore, we established normal age and sex related data for urinary calcium oxalate saturation in infancy and childhood to allow a more specific prediction of the risk of (recurrent) stone disease. MATERIALS AND METHODS: We collected 24-hour urine samples from 473 healthy infants and children without a history of renal stones. Urinary lithogenic and stone inhibitory substances were measured, and the urinary calcium oxalate saturation was calculated using a computer program. RESULTS: Mean urinary calcium oxalate saturation was always higher in boys than in girls, which was significant in infancy (5.22 versus 2.03, p < 0.05) and at ages 7 to 9 years (8.84 versus 5.47, p < 0.05). The saturation first increased (p < 0.05) until age 7 to 9 years in boys and girls, and remained at high levels at ages 10 to 12 years (7.03 versus 5.49, p < 0.05 compared to infancy). Calcium oxalate saturation then decreased until adolescence when values were comparable to those of infancy (5.29 versus 3.35). CONCLUSIONS: We recommend calculating urinary calcium oxalate saturation for diagnostic purposes as well as for therapy control. Normal age and sex related values must be considered.     

Sex- and strain-specific expression of cytochrome P450s in ochratoxin A-induced genotoxicity and carcinogenicity in rats

There is an urgent need for drugs capable of inhibiting renal calcifications, nephrocalcinosis and stones included, in humans. Current anticalcification medication is based mainly on alkalinization of the metabolism using potassium-containing citrate alone, despite the fact that calcium stone patients suffer marginally from both magnesium and potassium deficiency. We investigated the anticalcification efficacy of oral potassium citrate versus the combined administration of this drug and magnesium citrate in the magnesium-deficient rat developing corticomedullary nephrocalcinosis and luminal microliths in the long term. Among other things we employed specific stains for calcium and oxalate, light microscopy and element analysis for renal tissue and calcifications, respectively. In addition, minerals in renal tissue, urine and plasma were determined, as well as the state of extracellular calcium homeostasis. Magnesium deficiency caused pure calcium phosphate tissue deposits, containing no magnesium, but no deposition of calcium oxalate in the tubular lumen; tissue magnesium, calcium and phosphorus were increased, and there was marked potassium wastage via urine; despite mild hypercalcemia other signs of hyperparathyroidism were not found. Alkalinization with the two kinds of medication evoked an increase in urinary pH, citrate, and potassium; however, potassium citrate alone tended to aggravate renal concretions, whereas the combination of this drug with magnesium citrate completely prevented concretions. It was concluded that: (1) magnesium deficiency-induced calcifications are oxalate-free and are not sensitive to mobilization by alkalinization with potassium citrate, which might explain the failure of the drug to prevent stone recurrence in clinical stone patients, and (2) the combination of potassium citrate and magnesium citrate, which shows enormous anticalcification efficacy, deserves high priority in clinical trials aimed at evaluating strategies for the prevention of stones.     

Health care report cards

PURPOSE: A decreased concentration of magnesium in the urine is a risk factor for renal calcium stone disease that may be caused by decreased enteral absorption of magnesium. We analyze the possible reciprocal influences of enteral absorption of calcium and magnesium in patients with renal stone disease. MATERIALS AND METHODS: We measured the fractional enteral absorption of 47calcium and 28magnesium in 11 patients with renal calcium stone disease, including 8 with and 3 without hypercalciuria. Two tests were performed using calcium and magnesium, respectively, followed by another test in which the enteral absorption of calcium and magnesium was measured after both cations were administered together. RESULTS: We noted no clear influence of either cation on the absorption of the other in the 3 patients without hypercalciuria. However, in the 8 hypercalciuric patients enteral calcium absorption decreased after the concurrent administration of magnesium and enteral magnesium absorption increased after the concurrent administration of calcium. Each effect was proportional to the other. CONCLUSIONS: The results of this study indicate that the oral supplementation of magnesium in patients with hyperabsorptive hypercalciuria and renal calcium stone disease is favorable because it decreases calcium absorption and increases magnesium absorption. Both factors may reduce risk factors for renal calcium stone formation.     

Effects of citrate on the different phases of calcium oxalate crystallization

Urinary citrate appears to be an important factor in the crystallization process of calcium oxalate and calcium phosphate. The urinary excretion of citrate was found to be significantly lower in patients with calcium oxalate stone disease as compared with normal subjects, and about 30 per cent of the calcium stone formers can be considered as hypocitraturic. The lowest excretion of citrate was recorded in urine collected during the night. Citrate has significant effects on supersaturation with respect to both calcium oxalate and calcium phosphate, it also inhibits the growth of these crystals. In addition, citrate appears to be capable of inhibiting the aggregation of crystals composed of calcium oxalate, brushite, and hydroxyapatite. The heterogenous growth of calcium oxalate on calcium phosphate is also counteracted by citrate. As a consequence of the crucial role of citrate in these processes, stone prevention with alkaline citrate has become an attractive form of treatment in patients with recurrent stone formation. Single evening dose administration of sodium potassium citrate resulted in an of sodium potassium citrate resulted in an increased excretion of citrate, reduced levels of the calcium/citrate ratio as well as supersaturation with respect to calcium oxalate and a decreased rate of stone formation. However, conflicting results of stone preventive treatment with alkaline citrate have been reported by different groups, and long-term follow-up of patients treated in a randomized way is necessary to definitely assess the efficacy of alkaline citrate.     

Renal stones and primary hyperparathyroidism: natural history of renal stone disease after successful parathyroidectomy

The aim of the study was to evaluate the risk of renal stone recurrence after successful surgical treatment of primary hyperparathyroidism (pHPT). Of 297 consecutive patients with surgically verified pHPT, 151 patients had had renal stone disease; a total of 113 patients were eligible for follow-up; and of these, 107 patients remained normocalcemic during follow-up and formed the study group. The number of new stones were calculated by subtracting the stones present on preoperative urograms from the number of stones on urograms after 1, 3, and 5 years and the number of stones passed or eliminated by intervention. Among 107 patients, 32 (30%) formed one to four new stones within 5 years. This recurrence rate is comparable to the expected recurrence rate in idiopathic stone formers. Primary hyperparathyroidism and renal stone disease are common. As all renal stone formers are screened for pHPT by serum calcium analysis, the two diseases might by coincidence be found in the same patients. A considerable number of patients with pHPT and renal stone disease therefore experience recurrence of their stone disease irrespective of the presence of normocalcemia after successful parathyroidectomy.     

Pathogenesis of idiopathic calcium nephrolithiasis: update 1997

Idiopathic calcium nephrolithiasis (ICN) is a frequent disease in Western countries. The physicochemical theory of lithogenesis, which explains stone formation by the precipitation, growth, and crystalline aggregation of lithogenic salts in the urine, has contributed greatly to the understanding of the pathogenesis of calcium urolithiasis. However, several aspects are still unexplained; the co-existence of familial occurrence, primary tubular dysfunctions with ICN, and anomalies in the systemic handling of oxalate and calcium led to the development of a cellular hypothesis of ICN. A number of cellular defects in the handling of ions has been reported that involves both anion and cation transport. These anomalies are probably the expression of a still unknown cellular defect in idiopathic calcium stone formers. We suggested that an anomaly in the cell membrane composition might be responsible for the complex array of cell ion flux abnormalities observed in ICN. Recently, a disorder in the n-6 polyunsaturated fatty acid series has been described; it is characterized by a lower linoleic acid content and a higher arachidonic acid concentration in both plasma and erythrocyte membrane phospholipids of renal calcium stone patients. This anomaly could cause an increased activity of ion carriers; furthermore, it may lead to increased prostaglandin synthesis and to secondary phenomena at the kidney, skeletal, and intestinal level. As a consequence, critical conditions for lithogenesis in the kidney may ensue. The data suggest a common pathogenesis for hypercalciuria and hyperoxaluria. The systemic defect in the phospholipid arachidonic acid level may be both of dietary or genetic origin; experimental data suggest that the increase in delta-6 desaturase activity, the limiting enzyme in the metabolic pathway of polyunsaturated fatty acids, might be relevant to the pathogenesis of lipid abnormalities observed in nephrolithiasis and to the pathogenesis of ICN and its related problems (at the kidney, intestinal, and bone level).     

Uropontin in urinary calcium stone formation

Normal urine is frequently supersaturated with respect to calcium oxalate. Thus, urinary inhibitors of crystallization appear to have an important role in preventing urinary stone formation. Uropontin was isolated by monoclonal antibody immunoaffinity chromatography and has the same N-terminal sequence as osteopontin derived from bone. This urinary form of osteopontin is a potent inhibitor of calcium oxalate monohydrate crystal growth at concentrations (approximately 0.1 microM) that normally prevail in human urine. Interaction with calcium oxalate monohydrate in vivo was shown by analysis of EDTA extracts of calcium stones. Uropontin is an abundant component of calcium oxalate monohydrate stones and present in only trace quantities in calcium oxalate dihydrate and hydroxyapatite stones. However, the precise role of uropontin in the pathogenesis of urinary stone formation is not known and is the subject of ongoing investigations.     

Distribution of radioactivity from 14C-formaldehyde in pregnant mice and their fetuses

Fine structure, location and size of the core of 12 calcium oxalate monohydrate (COM) papillar calculi from different 'idiopathic' stone-formers were studied by an optical and scanning electron microscope equipped with the EDAX analytical device. Each individual core exhibited a unique overall structure composed of loosely arranged twined and intergrown crystals of plate-like and/or columnar shape and particles of 'rosette' structure with considerable void space among crystals in some cases or compact structure in others. Crystals were covered by a thin layer or organic material mostly invisible to the microscope. Sometimes debris of organic origin in a core was observed. A substantial amount of organic matrix appeared at the core boundary, often in the form of amorphous plates. The outer striated layer of COM stone consisting of tightly packed columnar crystals originated on this matrix. The stone core was located near the stone surface that was attached to the kidney wall and contained foreign particles that act as heterogeneous nucleants of calcium oxalate crystals.     

Prevalence of renal stones in a population-based study with dietary calcium, oxalate, and medication exposures

Little is known about the epidemiology of renal stones, in spite of the relative frequency of this painful condition. This population-based study examined reported renal stone diagnosis in 1,309 women aged 20-92 years to determine whether renal stones are associated with 1) food or water exposures or 2) lower bone mineral density and an increased likelihood of fractures. Results indicated a renal stone prevalence of 3.4%. The average age at diagnosis was 42 years. Renal stone formation was not associated with community of residence, hypertension, bone mineral density, fractures, high-oxalate food consumption, or ascorbic acid from food supplements. Women with renal stones consumed almost 250 mg/day less dietary calcium (p < 0.01) than did women without stones and had a lower energy intake (p < 0.04). The authors' findings do not support the hypothesis that increased dietary calcium is associated with a greater prevalence of renal stones, nor do they identify renal stones as a risk factor for low bone mineral density. Furthermore, lack of other identifiable environmental correlates and the relatively young age at initial diagnosis suggest that genetic components of renal stone formation need further study.     

Direct in vivo gene transfer to canine myocardium using a replication-deficient adenovirus vector

Inter-alpha-inhibitor (I alpha I) is a serine protease inhibitor present in human plasma. It has a molecular weight of about 220 kDa which encompasses 3 chains including two heavy chains and one light chain. The light chain, known as bikunin, is responsible for the antitryptic activity of I alpha I in the inhibition of various enzymes, such as trypsin and chymotrypsin. Under physiologic or certain pathologic circumstances, several macromolecules related to I alpha I appear in plasma and urine. However, the physiologic role of I alpha I remains unclear. As far as urolithiasis is concerned, two urinary macromolecules related to I alpha I have been isolated and shown to be potent inhibitors of calcium oxalate formation. One of these inhibitors, uronic-acid-rich protein (UAP), has been identified and well characterized. The sequence of the first 18 amino acid residues of UAP is identical with that of bikunin. Furthermore, the immunoreaction between UAP and I alpha I antibody using immunoblot analysis was positive. UAP isolated from the urine of stone formers exhibited less inhibitory activity towards calcium oxalate crystallization than that derived from the urine of healthy subjects. This suggests a structural abnormality of the inhibitor obtained from stone patients. The organic matrix extracted from kidney stones contained a protein antigenically related to I alpha I. We conclude that UAP is a member of I alpha I family taking part in inhibiting calcium oxalate crystallization, and modulating the formation of stones in the urinary tract.     

Thymocyte activation induces the association of phosphatidylinositol 3-kinase and pp120 with CD5

Specific anions in tubular fluid, including uropontin (UP), the urinary form of human osteopontin (OPN), block adhesion to renal tubular cells of the most common crystal in kidney stones, calcium oxalate monohydrate (COM). In this study, monkey renal epithelial cells (BSC-1 line) in monolayer culture constitutively secreted UP into the culture medium. COM crystals added to the medium avidly bound previously secreted UP, reducing its concentration by 46% one hour later. However, the net UP content of cultures after a 24-hour exposure to COM crystals was increased by 18%. Northern blotting showed that the constitutively expressed gene encoding human OPN was maximally stimulated in BSC-1 cells after exposure to COM crystals for 12 hours. Two other calcium-containing crystals, hydroxyapatite and brushite, did not alter OPN gene expression or protein production. OPN mRNA expression was enhanced in canine renal epithelial cells (MDCK line) after exposure to COM crystals for six hours, whereas the constitutive expression of murine OPN mRNA by 3T3 fibroblasts was unchanged. In vivo this glycoprotein could defend the cell against adhesion of crystals in tubular fluid, and/or promote renal interstitial fibrosis in subjects with heavy crystalluria.     

Sodium excretion in children with lithogenic disorders

INTRODUCTION: The causes of nephrolithisis are multifactorial and have not yet been enough investigated [1]. Hypercalciuria is the most common cause of metabolic nephrolithiasis [2-4]. Close relationship between urinary calcium and urinary sodium has been a subject of reported observations in the past, showing that high urinary sodium is associated with high urinary calcium [5-7]. Hyperoxaluria, hyperuricosuria and cystinuria are also metabolic disorders that can lead to nephrolithiasis. Recent studies have indicated that urinary elimination of cystine is influenced by urinary sodium excretion. Based on these observations it has been hypothesised that patients with high urinary sodium excretion are at high risk of urinary stone disease. The purpose of the study was to investigate sodium excretion in a 24-hour urine and first morning urine collected from children with lithogenic metabolic abnormalities (hypercalciuria, hyperoxaluria, hyperuricosuria, cystinuria), both with nephrolithiasis and without it, in order to determine its significance in urinary calculi formation. PATIENTS AND METHODS: Urinary sodium excretion was investigated in 2 groups of children: patients with lithogenic metabolic abnormalities, but without urinary stone disease (L group) and patients with nephrolithiasis (C group). Both groups were divided into 2 subgroups: patients with hypercalciuria and without it. There were 22 patients in group L (mean age 11.97 +/- 4.13 years), of whom 17 formed a hypercalciuric subgroup and 5 formed a non-hypercalciuric subgroup (3 patients with hyperuricosuria and 2 patients with hyperoxaluria). Group C consisted of 21 patients with nephrolithiasis (mean age 12.67 +/- 3.44 years), of whom 6 formed a hypercalciuric subgroup and 15 formed a non-hypercalciuric group (2 patients with cystinuria and 13 patients without lithogenic metabolic abnormalities). Control group consisted of 42 healthy age-matched children. All subjects had a normal renal function. A detailed history and clinical examination were done, and ultrasonography was performed in all patients. A 24-hour urine, first morning urine and serum specimen were analysed for sodium, potassium, calcium, uric acid, urea and creatinine. Fractional excretion of sodium, as well as urinary sodium to creatinin ratio and urinary sodium to potassium ratio, were calculated from the findings. Sodium and potassium levels were determined by flame photometry, calcium was measured by atomic absorption technique (Beckman Atomic Spectrophotometer, Synchron CX-5 model, USA), uric acid by carbonate method and creatinine by Jaffe technique. Cystine and dibasic amino acids were quantified by ion chromatography. Urinary oxalate excretion was determined by enzyme spectrophotometry. Hypercalciuria was defined by 24-hour calcium excretion greater than 3.5 mg/kg per day and/or calcium to creatinine ratio greater than 0.20 [8]. Uric acid excretion was expressed as uric acid excretion factored for glomerular filtration, according to Stapleton's and Nash's formula [9]. Normal values were lower than 0.57 mg/dl of glomerular filtration rate in 24-hour samples. Mean values were statistically analyzed by Pearson's linear correlation and analysis of variance (ANOVA). RESULTS: Urinary sodium concentration values including urinary sodium to potassium ratios, are shown in Table 1. We found that urinary sodium excretion was significantly increased in patients of both L and C groups when compared with controls (p < 0.05). Further analysis of the subgroups showed that urinary sodium excretion was significantly higher only in patients with hypercalciuria of both L and C groups in comparison to controls (p < 0.05) (Table 2). A significant positive correlation was found between 24-hour urinary sodium to creatinine ratio and urinary calcium to creatinine ratio (r = 0.31; p < 0.001) (Graph 1), as well as between urinary sodium to potassium ratio in 24-hour and first morning urine (r = 0.69; p < 0.001) (Graph 2). (A     

Effect of oral calcium loading on intact PTH and calcitriol in idiopathic renal calcium stone formers and healthy controls

The calciuric response after an oral calcium load (1000 mg elemental calcium together with a standard breakfast) was studied in 13 healthy male controls and 21 recurrent idiopathic renal calcium stone formers, 12 with hypercalciuria (UCa x V > 7.50 mmol/24 h) and nine with normocalciuria. In controls, serum 1,25(OH)2 vitamin D3 (calcitriol) remained unchanged 6 h after oral calcium load (50.6 +/- 5.1 versus 50.9 +/- 5.0 pg/ml), whereas it tended to increase in hypercalciuric (from 53.6 +/- 3.2 to 60.6 +/- 5.4 pg/ml, P = 0.182) and fell in normocalciuric stone formers (from 45.9 +/- 2.6 to 38.1 +/- 3.3 pg/ml, P = 0.011). The total amount of urinary calcium excreted after OCL was 2.50 +/- 0.20 mmol in controls, 2.27 +/- 0.27 mmol in normocalciuric and 3.62 +/- 0.32 mmol in hypercalciuric stone formers (P = 0.005 versus controls and normocalciuric stone formers respectively); it positively correlated with serum calcitriol 6 h after calcium load (r = 0.392, P = 0.024). Maximum increase in urinary calcium excretion rate, delta Ca-Emax, was inversely related to intact PTH levels in the first 4 h after calcium load, i.e. more pronounced PTH suppression predicted a steeper increase in urinary calcium excretion rate. Twenty-four-hour urine calcium excretion rate was inversely related to the ratio of delta calcitriol/deltaPTHmax after calcium load (r = -0.653, P = 0.0001), indicating that an abnormally up-regulated synthesis of calcitriol and consecutive relative PTH suppression induce hypercalciuria.(ABSTRACT TRUNCATED AT 250 WORDS)