2008部分英语考博试题--改错2008-10-30 00:29四、改错(1分×10=10分) mN'sJ1L-
NX?6
(lO,
d@{#F"o
2008部分英语考博试题--改错2008-10-30 00:29四、改错(1分×10=10分) ,-1d2y
_`xhP-,`S
BXUd
i&'O
The second most important constituent of the biosphere is o
X?~
*)Pb-c
liquid water. This can only exist in a very narrow range of temperatures, J|e3
UikA
r,wC5%&Za
since water freezes at 0°C and boils at 100°C. This is )9kp[hY
(YHK,aC>u
only a tiny range compared with the low temperatures of some ]O&yy{yYK
q5>!.v
other planets and the hot interior of the earth, let the temperature __1__ u\=yY.
pwo @
S"
of the sun. by controlpanel p
?x]|`M
hu:x,;`9H
As we know, life would only be possible on the face of a __2__ O,0j
+1?
<Mf(2`T
planet had temperatures somewhere within this range. __3__ ?cgb3^R'
!$fF3^8-
The earth’s supply of water probably remains quite fairly constant __4__ )D
':bWP
Ol*|J
in quantity. A certain number of hydrogen atoms, which #
0/,teJk
d>x(Bj6
are one of the main constituents of water, are lost by escaping W!
GUA<
+$B#] ,
from the atmosphere to out space, but they are probably just __5__ [ejl #'*5
(2r808^2
about to be replaced by new water rising away from the depths of the __6__ XF99h&;9
l"9$lF}
earth during volcanic action. The total quantity of water is not L7s
_3\
5} 1qo7;
known, and it is about enough to cover the surface of the globe __7__ >;k~B
ybpU?n
to a depth of about two and three-quarter kms. Most of it—97% ':|?M B
2yndna-
is in the form of the salt waters of the oceans. The rest is G/V0Yn""
YG>6;g)Zm
fresh, but three quarter of this is in the form of ice at the Poles __8__ -d6PXf5
IdciGS6t
and on mountains, and cannot be used by living systems when __9__ {)& b6}2h
PpR
eqm
o
melted. Of the remaining fraction, which is somewhat fewer __10__ (t"rzH
Ms=11C
than 1%of the whole, there is 10-20 times as much stored as underground )|<g\>/
@wa<nYd
water as is actually on the surface. There is also a minor,