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Introduction: A disturbed calcium-phosphate balance is an important issue for kidney stone formation in nephrolithiasis. Hypercalciuria (HC) has been proposed as an essential etiology of monosymptomatic nocturnal enuresis (MNE). Objectives: We may suspect that patients with MNE may be at risk of stone formation hence the objective of this paper was to assess the risk in MNE children using Bonn Risk Index (BRI). Patients and Methods: The urinary work-up of 204 children (83 with MNE and 121 controls) included urinary calcium (Ca), magnesium (Mg) and sodium (Na) excretion, Ca/creatinine ratio, BRI, ionized calcium (Ca2+), Mg/creatinine and Ca/citrate ratios, urinary citrates and oxalates (Ox). Results: Ca/creatinine and Mg/creat ratios were higher in the MNE group. There were no differences in Mg and Ca amount in urine and Mg/Ca ratio between MNE and the reference group. Both groups differed in Mg and Ca excretion per kg of body mass. MNE children differed from controls regarding BRI, Ox and urinary Ca2+. No differences in urinary citrate excretion nor Ca/citrate ratio between MNE and the controls were found. Correlations between factors important in the crystallization process in MNE children were recorded. Conclusion: MNE patients may be at risk of oxalate nephrolithiasis. Further studies to assess the role of the BRI and Ca/citrate ratio in predicting stone formation in MNE children are needed.

Introduction Although the age between the 6th and 12th months of life is considered to be optimal for the surgical treatment of cryptorchidism, a substantial part of the operations is carried out at a later age. Objective To evaluate the incidence of acquired cryptorchidism in boys who were operated upon on completing 3 years of age. Material and methods In the years 2010–2013 at the University Children's Hospital in Bialystok 328 orchidopexies in 318 boys were performed. 61.6% of the procedures were carried out after completion of 3 years of age. Results 19% of the boys who have orchidopexies carried out after 3 years of age had not been qualified for surgical treatment during the first examination because testes could be manipulated into the scrotum. After 1.5 to 11 years (mean 2.8 year) from the first visit, they were subjected to surgical treatment because gonads could no longer be moved to the scrotum. Conclusions Acquired cryptorchidism was documented in 19% of the boys operated after 3 years of age. This phenomenon explains a significant number of orchidopexies performed in older boys.

High fluid intake has been universally recommended for kidney stone prophylaxis. We evaluated 24-h urine osmolality regarded as the best biomarker of optimal hydration and upper metastable limit osmolality after water evaporation from urine sample to the onset of spontaneous crystallization and its usefulness as a new risk index that would describe an individual lithogenic potential. We collected 24-h urine from 257 pediatric patients with kidney stones and 270 controls. After volume and osmolality assessment, the urine samples were subjected to volume reduction in vacuum rotavapor continued to the onset of an induced urinary crystallization. The upper metastable limit osmolality of urine sample was calculated based on its initial osmolality value and the amount of water reduction. Pediatric stone formers presented with higher urine volume and lower urine osmolality than healthy controls. Despite that, their urine samples required much lower volume reduction to induce the spontaneous crystallization than those of controls. The ROC analysis revealed an AUC for the upper metastable limit osmolality of 0.9300 (95% CI 0.9104-0.9496) for distinguishing between stone formers and healthy subjects. At the cutoff of 2696 mOsm/kg, the test provided sensitivity and specificity of 0.8638 and 0.8189, respectively. 24-h urine osmolality provided the information about current hydration status, whereas evaporation test estimated the urinary potential to crystalize dependent on urine composition. Upper metastable limit osmolality may estimate the individual lithogenic capability and identify people at risk to stone formation when exposed to dehydration.

The Bonn Risk Index has been used to evaluate the risk of urinary calcium oxalate stone formation. According to the original method, risk should be determined based on 24-hour urine collection. We studied whether the Bonn Risk Index could be measured in spot urine samples and which part of the day is most suitable for this purpose.We collected total and fractionated 24-hour urine (in a 6-hour nocturnal portion and 9 consecutive 2-hour diurnal samples) in 42 children and adolescents with calcium oxalate urolithiasis and 46 controls. Bonn Risk Index values determined from each of the urine fractions were compared to those obtained from related 24-hour urine collections.Both groups exhibited similar circadian patterns of Bonn Risk Index values. Median Bonn Risk Index for the nighttime portion of urine in the stone group was 1.4 times higher than that obtained from the total 24-hour urine. The morning hours between 08:00 and 10:00 showed the peak lithogenic risk, and this fraction had the highest sensitivity and selectivity regarding discrimination between stone formers and healthy subjects. The afternoon hours demonstrated lower and less fluctuating crystallization risk. Despite diurnal fluctuations in Bonn Risk Index, there was still a well-defined cutoff between the groups.Bonn Risk Index determined from urine samples collected between 08:00 and 10:00 appears optimal in separating stone formers from healthy subjects, and appears as useful as the value determined from 24-hour urine collection. Investigation of this diurnal sample simplifies diagnosis in pediatric stone disease without loss of clinical information.

Purpose: The Bonn Risk Index has been used to evaluate the risk of urinary calcium oxalate stone formation. According to the original method, risk should be determined based on a 200 ml urine sample taken from a 24-hour collection. We evaluated whether the Bonn Risk Index can also be effectively determined in small urine samples. Materials and Methods: We studied 190 children and adolescents with nocturia and calcium oxalate urolithiasis. Initially Bonn Risk Index was determined according to the original method of Laube. Subsequently Bonn Risk Index was calculated using a computer program controlling a specially designed system to define the time point of induced crystallization based on consecutive urine samples of 1.5, 2.0 and 3.0 ml. Results: No significant differences were found in Bonn Risk Index between values obtained from 200 ml samples and those based on the micromethod with urine samples of 2 and 3 ml. Conclusions: Assessment of risk of urinary calcium oxalate stone formation with Bonn Risk Index in small urine volumes, based on prototype equipment controlled by specialized computer software, is comparable to the original method. This finding facilitates the procedure and improves Bonn Risk Index determination in children.

Cel pracy Określenie czestości wystepowania zmian nowotworowych i nienowotworowych u dziewczynek ze zmianami torbielowatymi i guzami jajnikow. Material i metody W Klinice Chirurgii Dzieciecej AMB w latach 2001–2006 leczono 36 dziewczynek z powodu rozpoznanych badaniem USG zmian torbielowatych jajnikow. Autorzy omawiają badania diagnostyczne, leczenie zachowawcze oraz wskazania do leczenia operacyjnego. Przedstawiają odlegle wyniki leczenia zachowawczego. Wyniki W grupie 36 dziewczynek u 24 (66%) stwierdzono proste torbiele jajnika, u 12 (34%) stwierdzono zmiany nowotworowe jajnika, u 10 (84%) byly to zmiany lagodne. 11 (48%) dziewczynek z torbielami jajnika wymagalo leczenia chirurgicznego. Wnioski W naszym materiale wiekszośc zmian w jajnikach u dziewczynek stanowily proste torbiele. Wśrod zmian nowotworowych przewazaly zmiany o charakterze lagodnym. Rokowanie u dziewczynek jest zwykle dobre, nawet w przypadkach zaawansowanych zmian nowotworowych. Postepowanie terapeutyczne powinno byc dobrane indywidualnie i uwzglednic zachowanie plodności. Resekcja macicy i totalna omentektomia w kazdym przypadku zlośliwego guza jajnika nie są konieczne u dzieci.

Aim There is conflicting evidence about the role of obesity in paediatric nephrolithiasis. This Polish study explored the influence of nutritional status and lipid disturbances on urinary lithogenic factors and the risk of kidney stone formation in children and adolescents from three to 18 years of age. Methods We carried out serum lipid profile evaluations and 24-h urine chemistry analyses on 493 overweight/obese paediatric participants (mean age 13 years) without nephrolithiasis and 492 healthy normal weight sex and age-matched controls. Results A third (33%) of the study group had blood lipid disturbances, with more acidic urine, lower urinary citrate excretion and a higher fraction of ionised calcium and higher Bonn Risk Index than the controls. The participants' body mass index standard deviation score (BMI Z-score) was positively correlated with urinary oxalate and uric acid and negatively correlated with citrate excretion. Total cholesterol, low-density lipoprotein cholesterol and triglycerides correlated negatively with citraturia, while high-density lipoprotein cholesterol correlated positively. Conclusion The main factor that predisposed overweight and obese children to kidney stones was hypocitraturia. Urinary citrate excretion was related to both BMI Z-scores and all lipid fraction abnormalities. However, hypercholesterolaemia and particularly low-density lipoprotein hypercholesterolaemia seemed to play a major role.

Streszczenie Przedstawiamy przypadek uchylka osierdzia wykryty przypadkowo na zdjeciu radiologicznym klatki piersiowej u 10-letniego chlopca. Badanie tomografii komputerowej i echokardiografii wykazalo obecnośc okrąglej, jednokomorowej torbieli polozonej w lewym kącie sercowo-przeponowym. Zmiana nie powodowala wowczas objawow klinicznych i jej leczenie chirurgiczne zostalo odroczone. W wieku 16 lat chlopiec zacząl skarzyc sie na bol w klatce piersiowej zlokalizowany przymostkowo i uczucie rozpierania w nadbrzuszu w czasie wysilku. Podczas torakoskopowego usuwania zmiany uwidoczniono jej komunikacje z workiem osierdziowym. Po jej usunieciu zglaszane przed zabiegiem dolegliwości calkowicie ustąpily. Badanie histopatologiczne wykazalo cienką, lącznotkankową ściane wyslaną mezotelium.

Idiopathic hypercalciuria is the most important predisposing risk factor for calcium oxalate (CaOx) renal stone formation. We assessed the associations between spontaneous CaOx crystallization based on the Bonn Risk Index (BRI), urinary pH, calciuria, oxaluria, and citraturia in 140 Caucasian patients with hypercalciuria, aged 4-17 years, and compared the findings with those in 210 normocalciuric controls. Of the 140 hypercalciuric patients, 58 had renal stones, and 82 had recurrent erythrocyturia, renal colic, or urinary obstructive symptoms-but without stones. Urinary ionized calcium ([Ca(2+)]) levels were measured using a selective electrode, while the onset of crystallization was determined using a photometer and titration with 40 mmol/L ammonium oxalate (Ox(2-)). The calculation of the BRI was based on the [Ca(2+)]:Ox(2-) ratio. The BRI values were 12-fold higher in hypercalciuric children than in healthy controls, but no differences were found in the BRI between subjects with urinary stones and those with urolithiasis-like symptoms. An increased BRI suggested an association with hypercalciuria, lower urinary pH, hypocitraturia, and hypooxaluria. These data indicate that hypercalciuria is an important factor associated with increased urinary CaOx crystallization, although the causal pathways need further investigation. Determination of the BRI in children with hypercalciuria may improve the risk assessment of kidney stones.

Objective To determine kidney stone composition in children and to correlate stone fractions with urinary pH and metabolic urinary risk factors. Patients and methods We studied 135 pediatric patients with upper urinary tract lithiasis in whom excreted or extracted stones were available for analyses. Composition of stones was analyzed. A 24-hour urine assessment included volume, pH and daily excretions of calcium, oxalate, uric acid, cystine, creatinine, phosphate, magnesium and citrate. Results Calcium oxalate was the major component of 73% stones, followed by struvite (13%) and calcium phosphate (9%). Uric acid was present in almost half of stones, but in rudimentary amounts. The calcium oxalate content in calculi showed a strong relationship with calciuria, and moderate association with oxaluria, magnesuria and acidification of urine. The percent content of struvite presented reverse and lower correlations with regard to the above parameters. Calcium phosphate stone proportion had low associations with urinary risk factors. Conclusions Calciuria, oxaluria, magnesuria and low urine pH exerted the biggest influence on calcium oxalate content in pediatric renal stones. Relationships of urinary risk factors with calculi calcium phosphate content were of unclear significance. Urinary citrate excretion did not significantly correlate with kidney stone composition in children.