首页> 外文期刊>地学杂志 >富士山北西斜面御庭付近のカラマツ低木林はなぜ維持されるのだろうか?一御中道巡りの魅力の再認識のために一
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富士山北西斜面御庭付近のカラマツ低木林はなぜ維持されるのだろうか?一御中道巡りの魅力の再認識のために一

机译:为什么要维护富士山西北坡花园附近的松松灌木林?重申一中中道之旅的魅力

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Mount Fuji is a relatively young mountain, which erupted intermittently until 1707. The tree limit on Mount Fuji is composed of larches (Larix leptolepis). The limit ranges from 1,400 to 2,900 meters in altitude, depending on the slope. Around Oniwa on the northwestern slope of Mount Fuji, a larch scrub community is scattered in patches, forming an island, where the tree line is 2,650 meters. All of the larches are severely deformed toward the northeast due to strong winds. Factors maintaining the larch scrub are examined referring to tree size and tree age. Tree size decreases rapidly above an altitude of 2,390 meters on the northwestern slope, where the forest limit is located. On this slope, we can observe both a group of trees showing a stronger tendency toward growth in terms of height and another group growth in terms of diameter. These growth patterns change depending on the altitude; that is, the higher the altitude, the greater the diameter, and the lower the altitude, the greater the height. On the other hand, the relationships between tree size and tree age show a tendency at lower altitudes of older trees having greater heights, and at higher altitudes of older trees having greater diameter, but not heights. These facts suggest that a larch scrub community forms by controlling exposure to the severe environment. This is also in accord with the observation of older trees having greater deformation. It is considered that embolism is a plausible cause controlling tree size, especially tree height, because frost action with severe transpiration frequently occurs on this slope. As a result, a scrub formation would be fixed. This explanation of the growth mechanism of the landscape around Oniwa on the northwestern part of the Ochu-do trail running along the side of Mount Fuji will assist eco- and geo-tourism development on the Ochu-do.
机译:富士山是一个相对年轻的山脉,断断续续地爆发直到1707年。富士山的树限由落叶松(Larix leptolepis)组成。根据海拔高度的不同,极限范围为海拔1,400至2,900米。在富士山西北坡的Oniwa周围,落叶松灌木丛散布在一块片上,形成了一个小岛,林线长2650米。由于强风,所有的幼虫都向东北严重变形。参照树木的大小和树龄来检查维持落叶松灌木丛的因素。在森林限制所在的西北坡海拔2390米以上,树木的大小迅速减小。在此坡度上,我们可以观察到一组树木在高度方面显示出更强的生长趋势,而在直径方面则显示出另一组。这些生长方式根据海拔高度而变化。即,海拔越高,直径越大,海拔越低,高度越大。另一方面,树的大小和树龄之间的关系在具有较高高度的老树的较低海拔处和具有较大直径但没有高度的老树的较高海拔处显示出趋势。这些事实表明,落叶松灌木丛通过控制暴露于恶劣环境而形成。这也与观察具有较大变形的老树相一致。认为栓塞是控制树木大小,尤其是树木高度的合理原因,因为在该斜坡上经常发生具有严重蒸腾作用的霜冻作用。结果,磨砂地层将被固定。这种对沿着富士山一侧延伸的奥丘道西北部Oniwa周围景观生长机制的解释,将有助于奥丘道的生态和地质旅游发展。

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