托福阅读新真经模考三

分享小红书,免费领会员
Font Size: 默认
  • Font Size:默认
  • Font Size:14px
  • Font Size:20px
  • Font Size:16px
  • Font Size:18px

Question 8 of 10

收藏本题
According to paragraph 4. which of the following is NOT true of false rings?

A. They are also called double rings.

B. Their exact cause is unknown.

C. They are very often mistaken for true rings even by experienced dendrochronologists

D. They consist of a strip of dark wood in the middle of a section of springwood.

Paragraph 4 is marked with []

我的答案 C 正确答案 C

本题用时3s
  • 官方解析
  • 网友贡献解析
  • 题目讨论
  • 标签
    0 感谢 0 不懂
    解析


    【答案】C

    【题型】否定事实信息题

    【解析】题干问的是关于“false rings”哪个选项不正确,提问内容比较广泛,且关键词在文段首句就出现,所以需要先看选项,关键词笔记如下:

    A. double rings

    B. cause?

    C. 认为true

    D. dark,spring中

    根据原文第一句对false ring的描述“...made of latewood that's in the middle of springwood.”说的是false ring是由位于springwood中间的latewood构成的,基本可以对应选项D,选项中的“a strip of dark wood”就是latewood的改写,可以根据上段内容以及上一题得知,并且后一句中也再次提到过“THE unusual dark ring”。

    继续第二句“These features, sometimes known as double rings...”可以排除选项A。另外这一句的主干说的是“这些特征通常能够和真的年轮区分开来”,与选项C的内容完全相反,所以这道题答案就是C选项。然后根据最后一句“It is not clear what creates such double rings...”可以排除选项B。

    综上答案为C。

  • 题目讨论

    如果对题目有疑问,欢迎来提出你的问题,热心的小伙伴会帮你解答。

译文
Challenge of Dendrochronology

Dendrochronology is the technique of counting tree rings to determine a tree's age and measuring the width of these rings to determine characteristics of past climates. This might seem simple: each ring represents one year, and wider rings generally mean better growing conditions-plentiful rainfall, moderate temperatures, and so forth. But the seasonal growth of a particular tree is affected by factors other than the weather. Trees vary, one from another, just like people do. The genetic makeup of each individual tree is unique, so one particular tree may grow a bit more quickly that another. Highly local conditions can also change over time. It is easy enough to see that if part of the soil near a tree has been eroded, this will impact the tree's root system and limit its growth, at least until the situation stabilizes. Then again, an infestation of insects may affect a tree in one valley more than the same type of tree ten miles away. Or one tree may suddenly start to get a lot more sunlight when an old, big tree in the neighborhood finally falls. These kinds of factors produce significant variations among individual specimens, and that fact means that researchers need to average together samples from many specimens of a single tree species in one region over the same time period. Some dendrochronologists think that measuring an average of twenty-five to thirty tree-ring records in a locale is an essential first step in getting around the problem of individual variability. While it may be easy enough to find thirty samples in some locations for particular periods, it obviously becomes less and less likely the more ancient the wood samples are.

/

Another issue is more general. Trees that are fortunate enough to live on good soil and near local sources of groundwater often grow at steady rates. Such growth translates into attractive trees that are tall and well formed; they also have rings that are wide and quite uniform in thickness, but their uniform growth rings make them entirely useless when it comes to inferring anything about past weather patterns. That is why, instead of looking at superb botanical specimens, dendrochronologists focus their work on wood from trees that are living a tough life due to poor soil, steep slopes, the absence of local groundwater, or some other challenge. It is these "tortured" trees that are the most likely to grow very little during years of scarce rains or do poorly after a harsh winter and a late spring. What this means, of course, is that few trees in the woods are likely to be good samples for the scientist. Indeed, it may be quite a small fraction that yields useful ring patterns. Again, this increases the challenge of finding enough good samples to say with much certainty what past conditions were like.

Another factor of dendrochronology relates to wood itself. In the spring, a tree grows rapidly, creating new cells on the outside of its trunk and branches, just under the bark. These cells, called "earlywood" or "springwood," are large and have thin cell walls; both these factors contribute to making the wood relatively lightweight for its volume. In the summer, growth slows. Denser "latewood" is formed, creating the band that is relatively dark when you look at the end of a piece of lumber. But occasionally the sequence of a perfect pair of springwood and latewood does not hold up. If conditions-weather or disease-severely test a tree one year, it will not grow over all its surfaces. That may mean that a particular sample of wood taken by the dendrochronologist will have a missing ring in it, which will result in the scientist's inferences being off base by a year

A few trees also may trip up scientists by revealing a "false ring" made of latewood that's in the middle of springwood. These features, sometimes known as double rings, usually can be distinguished from true rings because the unusual dark ring is likely to change gradually rather than more abruptly into the springwood that lies on either side of the false latewood. It is not clear what creates such double rings, although people have speculated that unusual conditions during the middle of the growing season or even highly local issues might be the cause.