Elucidation of the Origin of NOEs And ROEs that Show the Hydration in the Minor and Major Grooves of DNA Duplex with ATTAAT Tract by a Combination of NOESY and ROESY Experiments

Abstract

A combination of NOESY and ROESY experiments (using ammonia as a catalyst across the pH range of 5 to 8.6) has given us a clear understanding regarding the origin of nOes that are attributed to the stereochemical location and the residence time of water in the major and the minor grooves of d⁵'(¹C²C³A⁴T⁵T⁶A⁷A⁸T⁹G¹⁰G)₂ ³' duplex Our conclusions are the following: (i) In the major groove, the presence of ammonia in the buffer does not influence on the process of exchange between bound and bulk water, (ii) It has been found that the observation of the bound water in the minor groove is a result of straight dipole-dipole effect at the physiological pH. (iii) The residence time of water near H2 of adenine (H2A) in the minor groove has been estimated to be in the range of 0.3–0.5ns, which is closer to the residence time of the bound water found on the surface of protein, (iv) The hydration pattern in the minor groove in the physiological pH, under our NMR measurement condition, is similar to the ones found in the X-ray structure, (v) It has been shown that at pH > 8.0 the nOe/rOe intensities of the water-H2A crosspeaks dramatically increase due to dipole-dipole and/or relayed magnetization transfer from H2A to water through ammonia catalyst.