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DƯỢC LÍ Goodman & Gilman's The Pharmacological Basis of Therapeutics 12th, 2010

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1276

10

9

2.5

Intestine:

800 mg intake

Bone:

8

7

protein bound

40%

2.0

300 mg

300 mg

SECTION V

Total calcium

mg/dl

6

5

4

3

2

complexed

10%

ionized

50%

1.5

1.0

0.5

mM

Diffusible calcium

300 mg absorbed

150 mg endogenous loss

Kidney:

9000 mg filtered

8850 mg reabsorbed

HORMONES AND HORMONE ANTAGONISTS

1

0

0.0

Figure 44–1. Pools of calcium in serum. Concentrations are

expressed as mg/dL on the left-hand axis and as mM on the right.

The total serum calcium concentration is 10 mg/dL or 2.5 mM,

divided into three pools: protein-bound (40%), complexed with

small anions (10%), and ionized calcium (50%). The complexed

and ionized pools represent the diffusable forms of calcium.

The total plasma calcium concentration can be

interpreted only by correcting for the concentration of

plasma proteins. A change of plasma albumin concentration

of 1.0 g/dL from the normal value of 4.0 g/dL

can be expected to alter total calcium concentration by

~0.8 mg/dL.

The extracellular Ca 2+ concentration is tightly

controlled by hormones that affect calcium entry at the

intestine and its exit at the kidney; when needed, these

same hormones regulate withdrawal from the large

skeletal reservoir.

Calcium Stores. The skeleton contains 99% of total body calcium

in a crystalline form resembling the mineral hydroxyapatite

[Ca 10

(PO 4

) 6

(OH) 2

]; other ions, including Na + , K + , Mg 2+ , and F - , also

are present in the crystal lattice. The steady-state content of calcium in

bone reflects the net effect of bone resorption and bone formation, coupled

with aspects of bone remodeling. In addition, a labile pool of bone

Ca 2+ exchanges readily with interstitial fluid. This exchange is modulated

by hormones, vitamins, drugs, and other factors that directly alter

bone turnover or that influence the Ca 2+ level in interstitial fluid.

Calcium Absorption and Excretion. In the U.S., ~75% of dietary calcium

is obtained from milk and dairy products. The adequate intake

value for calcium is 1300 mg/day in adolescents and 1000 mg/day

in adults. After age 50, the adequate intake is 1200 mg/day. This contrasts

with median intakes of calcium for boys and girls ≥9 years of

age of 865 and 625 mg, respectively, and a median daily calcium

intake of 517 mg for women >50 years of age.

650 mg fecal loss

150 mg excreted

Figure 44–2. Schematic representation of the whole body daily

turnover of calcium. (Adapted with permission from Yanagawa

N, Lee DBN. Renal handling of calcium and phosphorus. In:

Disorders of Bone and Mineral Metabolism (Coe FL, Favus MJ,

eds.), Raven Press, New York, 1992, pp. 3–40.)

Figure 44–2 illustrates the components of whole-body daily

calcium turnover. Ca 2+ enters the body only through the intestine.

Active vitamin D–dependent transport occurs in the proximal duodenum,

whereas facilitated diffusion throughout the small intestine

accounts for most total Ca 2+ uptake. This uptake is counterbalanced

by an obligatory daily intestinal calcium loss of ~150 mg/day that

reflects the calcium content of mucosal and biliary secretions and in

sloughed intestinal cells.

The efficiency of intestinal Ca 2+ absorption is inversely related

to calcium intake. Thus, a diet low in calcium leads to a compensatory

increase in fractional absorption owing partly to activation of

vitamin D. In older persons, this response is considerably less robust.

Disease states associated with steatorrhea, diarrhea, or chronic malabsorption

promote fecal loss of calcium, whereas drugs such as glucocorticoids

and phenytoin depress intestinal Ca 2+ transport.

Urinary Ca 2+ excretion is the net difference between the quantity

filtered at the glomerulus and the amount reabsorbed. About 9 g of Ca 2+

are filtered each day. Tubular reabsorption is very efficient, with >98%

of filtered Ca 2+ returned to the circulation. The efficiency of reabsorption

is highly regulated by parathyroid hormone (PTH) but also is influenced

by filtered Na + , the presence of nonreabsorbed anions, and diuretic

agents (Chapter 25). Sodium intake, and therefore sodium excretion, is

directly related to urinary calcium excretion. Diuretics that act on the

ascending limb of the loop of Henle (e.g., furosemide) increase calcium

excretion. By contrast, thiazide diuretics uncouple the relationship

between Na + and Ca 2+ excretion, increasing sodium excretion but diminishing

calcium excretion (Friedman and Bushinsky, 1999). Urine Ca 2+

excretion is a direct function of dietary protein intake, presumably owing

to the effect of sulfur-containing amino acids on renal tubular function.

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