Effects of in vivo metabolic acidosis on midcortical bone ion composition

Citation
Da. Bushinsky et al., Effects of in vivo metabolic acidosis on midcortical bone ion composition, AM J P-REN, 277(5), 1999, pp. F813-F819
Citations number
60
Categorie Soggetti
da verificare
Journal title
AMERICAN JOURNAL OF PHYSIOLOGY-RENAL PHYSIOLOGY
ISSN journal
03636127 → ACNP
Volume
277
Issue
5
Year of publication
1999
Pages
F813 - F819
Database
ISI
SICI code
0363-6127(199911)277:5<F813:EOIVMA>2.0.ZU;2-O
Abstract
Chronic metabolic acidosis increases urine calcium excretion without alteri ng intestinal calcium absorption, suggesting that bone mineral is the sourc e of the additional urinary calcium. During metabolic acidosis there appear s to be an influx of protons into bone mineral, lessening the magnitude of the decrement in pH. Although in vitro studies strongly support a marked ef fect of metabolic acidosis on the ion composition of bone, there are few in vivo observations. We utilized a high-resolution scanning ion microprobe w ith secondary ion mass spectroscopy to determine whether in vivo metabolic acidosis would alter bone mineral in a manner consistent with its purported role in buffering the increased proton concentration. Postweanling mice we re provided distilled drinking water with or without 1.5% NH4Cl for 7 days; arterial blood gas was then determined. The addition of NH4Cl led to a fal l in blood pH and HCO3- concentration. The animals were killed on day 7, an d the femurs were dissected and split longitudinally. The bulk cortical rat ios Na/Ca, K/Ca, total phosphate/carbon-nitrogen bonds [(PO2 + PO3)/CN], an d HCO3-/CN each fell after 1 wk of metabolic acidosis. Because metabolic ac idosis induces bone Ca loss, the fall in Na/Ca and K/Ca indicates a greater efflux of bone Na and K than Ca, suggesting H substitution for Na and K on the mineral. The fall in (PO2 + PO3)/CN indicates release of mineral phosp hates, and the fall in HCO3-/CN indicates release of mineral HCO3-. Each of these mechanisms would result in buffering of the excess protons and retur ning the systemic pH toward normal.