We investigate the hydration dynamics of a sma
ll g
lobu
lar protein, hen egg-white
lysozyme. Extensive simu
lations (two trajectories of 9 ns each) were carried out to identify the time-sca
les and mechanism of water attachment to this protein. The
location of the surface and integra
l water mo
lecu
les in
lysozyme was a
lso investigated. Three pecu
liar tempora
l sca
les of the hydration dynamics can be discerned: two among these, with sub-nanosecond mean residence time, τ
w, are characteristic of surface hydration water; the s
lower time-sca
le (τ
w![]()
lign=center border=0 SRC=/images/g
lyphs/BQ1.GIF>2/3 ns) is associated with buried water mo
lecu
les in hydrophi
lic pores and in superficia
l c
lefts. The computed τ
w va
lues in the two independent runs fa
ll in a simi
lar range and are consistent with each other, thus adding extra weight to our resu
lt. The τ
w of surface water obtained from the two independent trajectories is 20 and 24 ps. In both simu
lations on
ly three water mo
lecu
les are bound to
lysozyme for the entire
length of the trajectories, in agreement with nuc
lear magnetic re
laxation dispersion estimates. Locations other than those identified in the protein crysta
l are found to be possib
le for these
long-residing water mo
lecu
les. The dynamics of the hydration water mo
lecu
les observed in our simu
lations imp
lies that each water mo
lecu
le visits a mu
ltitude of residues during the
lifetime of its bound with the protein. The number of residues seen by a sing
le water mo
lecu
le increases with the time-sca
le of its residence time and, on average, is equa
l to one on
ly for the water mo
lecu
les with shorter residence time. Thus, τ
w va
lues obtained from ine
lastic neutron scattering and based on jump-diffusion mode
ls are
like
ly not to account for the contribution of water mo
lecu
les with
longer residence time.