Page 130 - Color Atlas Of Pathophysiology (S Silbernagl Et Al, Thieme 2000)
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Urolithiasis
       Concrement-forming substances (→ A1) can  Abnormal renal reabsorption is a frequent
       reach concentrations in the urine that lie  cause of increased renal excretion in hypercal-
       above their solubility threshold. In the so-  ciuria and an invariable cause in cystinuria
       called metastable range the formation of crys-  (→ p. 96). The Ca 2+  concentration in blood is
       tals may not occur at all, or only slowly, despite  then maintained by the intestinal absorption
       supersaturation of the solution. However,  and mobilization of bone minerals, while the
       when the concentrations rise beyond the  cystine concentration is maintained by a re-
       metastable range, crystallization occurs. Dis-  duced breakdown.
    Kidney, Salt and Water Balance  kidney stones are calcium oxalate (ca. 70%),  urine concentration (→ A4).
       solving already formed crystals is possible
                                        Release of ADH (in volume depletion, stress,
       only by reducing the concentration to below
                                       etc.; → p. 260) leads to a raised concentration
                                       of stone-forming substances via enhanced
       the metastable range.
         The most frequently found components in
                                        The solubility of some substances depends
       calcium phosphate or magnesium-ammonium
                                       on the pH of urine. Phosphates are easily dis-
                                       solved in an acidic urine, but poorly in an alka-
       phosphate (ca. 30%), uric acid or urate (ca.
       30%) as well as xanthine or cystine (< 5%). Sev-
                                       line one. Phosphate stones are therefore, as a
                                       rule, only found in alkaline urine. Conversely,
       eral substances may be contained in one stone,
                                       ated than undissociated, and uric acid stones
       as nuclei for crystallization and facilitate the
       deposition of other metastably dissolved sub-
                                       are formed more readily in acidic urine. If the
                                       formation of NH 3 is reduced, the urine has to
       stances (hence the total is > 100%).
    5  because crystals that have already formed act  uric acid (urate) is more soluble when dissoci-
         Certain substances that form complexes,  be more acidic for acid to be eliminated, and
       such as citrate, pyrophosphate, and (acid)  this promotes the formation of urate stones.
       phosphate, can bind Ca 2+  and, by reducing the  A significant factor is also how long crystals
       Ca 2+  concentration, are able to prevent calcium  that have already formed actually remain in
       phosphate and calcium oxalate from precipi-  the supersaturated urine. The length of time
       tating.                         depends on the diuresis and the flow condi-
         Causes of stone formation. The raised con-  tions in the lower urinary tract that can, for ex-
       centration of stone-forming substances can be  ample, lead to crystals getting caught (postre-
       the result of prerenal, renal, and postrenal fac-  nal cause).
       tors:                            The effect of urolithiasis is that it blocks the
         Prerenal causes produce the increased filtra-  lower urinary tract (→ A5). In addition,
       tion and excretion of stone-producing sub-  stretching of the ureteric muscles elicits very
       stances via a raised plasma concentration  painful contractions (renal colic). Obstruction
       (→ p. 94). Thus, prerenal hypercalciuria and  to flow leads to ureteral dilation and hydrone-
       phosphaturia are the result of raised intestinal  phrosis with cessation of excretion. Even after
       absorption or mobilization from bone, for ex-  removal of a stone, damage to the kidney may
       ample, if there is an excess of PTH or calcitriol  persist. The urinary obstruction also promotes
       (→ A2). Hyperoxalemia can be brought about  growth of pathogens (urinary tract infection;
       by a metabolic defect in amino acid break-  pyelonephritis; → p.106). Urea-splitting patho-
       down or by increased intestinal absorption  gens form NH 3 from urea, thus alkalinizing the
       (→ A3). Hyperuricemia occurs as a result of  urine. This in turn, in a vicious circle, favors the
       an excessive supply, increased new synthesis,  formation of phosphate stones. Even without
       or increased breakdown of purines (→ A3).  bacterial colonization, intrarenal deposition of
       Xanthine stones may occur when the forma-  uric acid (gouty kidney) or of calcium salts
       tion of purines is greatly increased and the  (nephrocalcinosis) can result in inflammation
       breakdown of xanthines to uric acid is inhib-  and destruction of renal tissue.
       ited. However, xanthine is much more soluble
  120  than uric acid and xanthine stones are there-
       fore much less common.
       Silbernagl/Lang, Color Atlas of Pathophysiology © 2000 Thieme
       All rights reserved. Usage subject to terms and conditions of license.
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