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Question 7 of 10

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According to paragraph 3, which of the following is NOT true of earlywood?

A. It is less dense than latewood

B. It makes up the part of the ring that appears dark

C. Its cells are large with thin walls

D. It forms quickly, just under the bark of the tree's trunk and branches.

Paragraph 3 is marked with []

我的答案 B 正确答案 B

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    解析


    【答案】B

    【题型】否定事实信息题

    【解析】题干问的是哪个关于earlywood的信息不正确,否排题可以先看选项后再回原文。选项关键词笔记参考如下:

    A. dense<latewood

    B. →dark ring

    C. 大cell 薄wall

    D. 快,bark下

    根据原文第二句话“In the spring...”,说的是“在春天一棵树迅速生长,在它的树干和树枝的外面,在树皮下产生新的细胞。” 后一句出现了题干定位词,也就是这些细胞叫作earlywood或者springwood,它们很大并且细胞壁很薄。根据这两句信息可以排除选项C和D。后面一句“In the summer...”开始说到,夏天的时候生长变慢,Denser "latewood" is formed 这句可以对应选项A说earlywood比latewood密度更低,排除A。综上答案为B,选项B说的dark ring不是题干问的earlywood,而是“latewood”部分的特征,原文说的是“密度更大的latewood形成了,构成颜色较暗的条带,当你看一块木材尾部时就可以看到”,所以选项B为答非所问。

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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.

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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.