The second most important constituent of the biosphere is
+ [4 R& S' m$ S5 Q" y! I: u/ | liquid water. This can only exist in a very narrow range of temperatures,% \2 B( t, v* ]5 h" z! O% G: H
since water freezes at 0°C and boils at 100°C. This is I6 C! b/ e. ~; a" G' Z) U1 w
only a tiny range compared with the low temperatures of some
1 k2 m, ]% U4 F. a+ r0 A. P other planets and the hot interior of the earth, let the temperature __1__
1 J; | Q4 ~4 } of the sun.
4 ~% d9 j; K* \+ M2 @9 |; i, ? As we know, life would only be possible on the face of a __2__
/ ]+ R8 R# z M. ` @' ]& t planet had temperatures somewhere within this range. __3__
$ H& C$ o* f( D+ v$ _" T& T The earth’s supply of water probably remains quite fairly constant __4__
9 r8 c1 P. `7 U$ ^/ I; R+ w7 O7 b in quantity. A certain number of hydrogen atoms, which
) v3 M0 P+ h; v6 `+ s are one of the main constituents of water, are lost by escaping
/ R( g3 N8 t+ ` from the atmosphere to out space, but they are probably just __5__
2 p# }* x+ }" @+ X3 ^, a0 Q about to be replaced by new water rising away from the depths of the __6__
# J% e" T4 S7 N* {# g# \ earth during volcanic action. The total quantity of water is not( l1 t! A" [( I3 \' b1 P
known, and it is about enough to cover the surface of the globe __7__
' X7 G" d' C9 j: ~9 _: j7 n/ m to a depth of about two and three-quarter kms. Most of it—97%
- ^! ~" K9 i) h- v9 [# u is in the form of the salt waters of the oceans. The rest is. \8 O& i+ q, S* V5 b
fresh, but three quarter of this is in the form of ice at the Poles __8__% D$ j# f5 y! h
and on mountains, and cannot be used by living systems when __9__' J5 a$ \% s9 Y3 J q3 C/ R( @
melted. Of the remaining fraction, which is somewhat fewer __10__" }) \2 B, p3 E0 C( w. I9 r$ r
than 1%of the whole, there is 10-20 times as much stored as underground- v: m+ o& u, d1 j
water as is actually on the surface. There is also a minor,/ f( G3 l$ q# k' g2 K1 t; N
but extremely important, fraction of the water supply& ^8 C x( K2 m9 N, |3 F6 d
which is present as water vapour in the atmosphere.4 B. v1 @3 L; m2 T) e& d9 m1 i
答案:
0 E& ]; S( D! l: e 1.Let ^the 加入alone. Let alone 意为“更不用说”, 表示一种让步关系。
$ d- Q3 q7 P3 X# q8 I) [6 u 2.face-surface 根据上下文理解,应该指地球的表面。, [3 G1 Y' L, R& N6 q
3.planet^had 加入which或that。这样使得planet后面的句子成为一个定语从句。
# q! S- R8 t; E$ h, c3 _ 4.去掉fairly或quite 意思重复。
# }- t' E6 N* ~7 m5 X4 [ 5.out改成outer 这里指外层空间。8 T! b. [8 X7 S
6.去掉away rise后面不接away。
' S; B8 M$ b, b$ a: k. U) o2 y 7.and改成although 短文中这里是让步关系,而不是并列关系。" F q I' z D! r" s, q
8.quarter改成quarters 英语表达中,当分子是二以上的数时,分母应为复数。. ~4 V9 K) l. @6 x' {& y8 h
9.when改成until或者unless 根据上下文,这句话的意思应为:除非(冰雪)融化,否则(地球上的)生命系统就无法利用水。所以when在这里的意思有误。 p) u' h. p6 ~7 l! z
10.fewer改成less 文中的remaining fraction 仍指水,因此不能用fewer,要用less。 |