The Study of Climate under the Ground The Observation on the Depth and Temperature of hotherthal Stratum in Japan & Manchuria
The Study of Climate under the Ground The Observation on the Depth and Temperature of hotherthal Stratum in Japan & Manchuria
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地下气候研究 日本霍瑟塔尔地层深度和温度观测
DOI：
10.5026/jgeography.59.88
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发表时间：
1950
影响因子：
3.1
通讯作者：
Shirobee Kiuchi
中科院分区：
文献类型：
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作者：
Shirobee Kiuchi
作者对日本和满洲等温地层的深度和温度的分布进行了研究，发现等温地层的深度和温度一般是纬度的函数，高纬度地区的等温地层深度比低纬度地区浅，温度也低。日本的深度为10-16 m，满洲的深度为10-14 m。日本的气温为8-18°C，满洲为2-11°C。这种现象的原因被认为是由于冬季地表地层结冰所致。但有几个地区的温度受到覆盖植物、土壤性质和含水量的干扰。等温温度。从地球物理学的角度来看，地层非常重要。它将为断层、地流和地磁的研究提供一把钥匙。此外，它对于农业气候也具有重要意义，作者将在下面的论文中将其作为“土柱上部等温地层的热变化研究”来完成。
The author studied on the distribution of the depth and temperature of isothermal stratum in Japan and Manchuria, He observed that the depth and temperature of isothermal stratum are generally the function of latitude, and then its depth is shallower and its temperature is lower in high latitude than in low latitude. Its depth is 10-16 m in Japan and is 10-14 m in Manchuria. Its temperature is 8-18°C in Japan and is 2-11°C in Manchuria.The reason of this phenomenon is thought to be due to the freezing at the surface stratum of the earth in winter. But there are several regions, where the temperatures are disturbed by the covering plant, the nature of soil and the moisture content.The temperature of isothermal. stratum is very important in the geophysical point of view. It will give a key to the study in fault, earth current and geomagnetism. Moreover it will have a significance in the agrar-climate, which the author will complete as “Studies on thermal change in a soil column upper isothermal stratum” on the following treatise.