Infrared spectroscopy was used to study DNA complexes with Ca2+ ions i
n films with different relative humidity at [Ca2+]/[P] molar ratios ra
nging from 0.4 to 20. It was shown that in complex with Ca2+ the DNA p
asses into the B form at a larger average number of water molecules bo
und per nucleotide (n = 18 at [Ca2+]/[P] = 10, n = 24 at [Ca2+]/[P] =
20, and n = 12 in the absence of Ca2+). Calcium ions cause a low-frequ
ency shift of the absorption band corresponding to the valence vibrati
ons of water sorbed on DNA. This evidenced stronger binding of water m
olecules in the hydration shell of the DNA-Ca2+ complex as compared wi
th free DNA. The results obtained confirm the previously proposed mode
l of the complex. The Ca2+ ions bind to theoxygen of the DNA phosphate
groups and to the N7 atom of guanine, forming chelate complexes of th
e N7-Ca2+-O6 type.