Although H2O has been the topic of considerable research since the beg
inning of the century, the peculiar physical properties are still not
well understood. We discuss recent experiments and simulations relatin
g to the hypothesis that, in addition to the known critical point in w
ater, there exists a ''second'' critical point at low temperatures. in
particular, we discuss very recent measurements of the compression-in
duced melting and decompression-induced melting lines of high-pressure
forms of ice. We show how knowledge of these lines enables one to obt
ain an approximation for the Gibbs potential G(P, T) and the equation
of state V/(P, T) for water, both of which are consistent with the pos
sible continuity of liquid water and the amorphous forms of solid wate
r. We also comment on some of the evidence that is equally consistent
with other scenarios for the behavior of liquid water. (C) 1998 Elsevi
er Science B.V. All rights reserved.