Method of Investigating Groundwater-vein Streams by Measuring One-meter-depth Temperature in Landslide Areas Part 1

A. Takeuchi
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引用次数: 15

Abstract

The occurrence of a landslide is very often correlated with topographical and geological characteristics of the landslide area as well as the existence of groundwater in the area. Therefore, overall information about surface and underground water in the landslide area is required in order to elucidate the mechanism of the slide, to predict its activity, and to design construction works for its prevention. On the basis of various findings and observations hitherto accumulated on groundwater in and outside landslide areas, the water may be divided into two categories ; the one flowing at a low filtration velocity through strata which are regarded hydrogeologically as aquifers, and the other flowing at considerably high filtration velocities through stratum portions, water veins which are distinguished in permeability from their surroundings. When the water veins postulated above are supplied with a large quantity of water at a stretch by a heavy rain or meltwater, or when abnormal effects are exercised on the veins by an earthquake, banking, or other causes, a possibility of landslide occurrence is developed. Therefore, in order to elucidate the above-mentioned mechanism etc., it is necessary to grasp the routes and scales of these water veins. The conditions of existence of groundwater in and outside landslide areas used to be investigated mainly by seismic and/or electrical methods which utilize either elastic or electrical properties of soil mass including water, respectively. These methods are useful to detect places where water may exist in a relatively large quantity. However, the both methods have furnished little information with regard to water existing in a vein form. Considering circumstances in summer that many landslide areas are rich in cold spring water and on the other hand the earth's surface is heated to a warmer temperature by solar radiation, the utilization of the temperature difference between them could offer useful information on the location and size of water vein. Reflecting upon the methods so far used, the author found out that methods utilizing thermal properties of water and soil are not included among them. Prospecting methods applying underground temperature measurement at shallow depth have been studied and employed mainly in the field of hot-spring exploration. YUHARA (1955) presented a method by which the scale and existence depth of a hot-spring vein are estimated theoretically from a temperature-distance curve obtained by measuring 1-m-depth underground temperature. Except for the field of hot-springs, NOMURA and MAKINO (1958) carried out preliminary investigations for mining by measuring temperature of shallow depth up to 60 cm, and examined the accuracy of ther-
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滑坡区一米深测温调查地下水脉流的方法第1部分
滑坡的发生往往与滑坡地区的地形、地质特征以及该地区是否存在地下水有关。因此,为了阐明滑坡的发生机制,预测滑坡的活动,设计防止滑坡的施工工程,需要掌握滑坡区地表水和地下水的全面信息。根据迄今为止对滑坡区内外地下水的各种发现和观测,可将其分为两类;一种以较低的过滤速度流过在水文地质学上被认为是含水层的地层,另一种以相当高的过滤速度流过地层部分,即在渗透率上与其周围环境不同的水脉。当暴雨或融水给上述假定的水脉提供大量的水时,或者当地震、河岸或其他原因对水脉产生异常影响时,就有可能发生滑坡。因此,为了阐明上述机制等,有必要掌握这些水脉的路线和规模。塌陷区内外地下水的存在条件过去主要通过地震和/或电学方法进行调查,这些方法分别利用包括水在内的土体的弹性或电学特性。这些方法对于探测可能存在相对大量水的地方很有用。然而,这两种方法都没有提供关于以脉状形式存在的水的信息。考虑到夏季许多滑坡区冷泉丰富,另一方面地球表面被太阳辐射加热到较高的温度,利用两者之间的温差可以提供有关水脉位置和大小的有用信息。回顾目前使用的方法,笔者发现利用水和土壤热性质的方法并不在其中。研究了利用地下浅层测温的找矿方法,主要应用于温泉勘探领域。YUHARA(1955)提出了一种从测量地下1 m深度温度得到的温度-距离曲线理论上估计温泉脉的规模和存在深度的方法。除了温泉领域外,NOMURA和MAKINO(1958)通过测量60厘米以下的浅层深度温度进行了采矿的初步调查,并检验了其准确性
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岩盤地下水の水質・同位体組成調査*(1) 特性曲線型有限要素法を用いた密度差のある地下水流動の数値解析-淡水・塩水2相流への応用 非定常地下水変動場における透水(量)係数の推定 A‘Characteristie’Finite Element Method for Dispersion-Convection Equation. The Fluctuation in Groundwater Level prior and after the Miyagi Oki Earthquakes.
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