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如前所述,冻土中未冻水的野外观测还没有可靠的技术。而现有资料中青藏沿线土的相关数据又太少,不足以支持本文的需要。因此,本文采用温度—未冻水关系函数来计算冻土中的未冻水含量...
如前所述,冻土中未冻水的野外观测还没有可靠的技术。而现有资料中青藏沿线土的相关数据又太少,不足以支持本文的需要。因此,本文采用温度—未冻水关系函数来计算冻土中的未冻水含量。未冻水含量和负温具有如下关系式[20]:
(2-6)
式中: 为未冻水含量,%; 为负温绝对值,℃;a和b为经验系数。
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(2-6)
式中: 为未冻水含量,%; 为负温绝对值,℃;a和b为经验系数。
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如前所述,冻土中未冻水的野外观测还没有可靠的技术。
As mentioned above, there is no reliable technology for the field observation of the unfrozen water in permafrost.
而现有资料中青藏沿线土的相关数据又太少,不足以支持本文的需要。
And currently there is little relevant data of permafrost along the Qinghai-Tibetan highway to serve this paper.
因此,本文采用温度—未冻水关系函数来计算冻土中的未冻水含量。
Hence, this paper adopt the temperature-unfrozen water function to calculate the unfrozen water content in permafrost.
未冻水含量和负温具有如下关系式[20]:
The relationship between the content of unfrozen water and the negative temperature can be expressed as below:
(2-6)
式中: 为未冻水含量,%; 为负温绝对值,℃;a和b为经验系数。
In this function, ~represents the content of unfrozen water,%;~ represents the absolute value of negative temperature,℃; a and b represent experience coefficients.
As mentioned above, there is no reliable technology for the field observation of the unfrozen water in permafrost.
而现有资料中青藏沿线土的相关数据又太少,不足以支持本文的需要。
And currently there is little relevant data of permafrost along the Qinghai-Tibetan highway to serve this paper.
因此,本文采用温度—未冻水关系函数来计算冻土中的未冻水含量。
Hence, this paper adopt the temperature-unfrozen water function to calculate the unfrozen water content in permafrost.
未冻水含量和负温具有如下关系式[20]:
The relationship between the content of unfrozen water and the negative temperature can be expressed as below:
(2-6)
式中: 为未冻水含量,%; 为负温绝对值,℃;a和b为经验系数。
In this function, ~represents the content of unfrozen water,%;~ represents the absolute value of negative temperature,℃; a and b represent experience coefficients.
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As stated above, not frozen water in permafrost field observation, there is no reliable technology. While the existing material in the relevant data along the soil and too small to support this paper needs. Therefore, in this article, the temperature-not cold water relations function to compute the permafrost is not cold water content. Not frozen water content and negative temperature has the following equation [20] : (2-6) Type: cold water content for not, %; For negative temperature absolute value, ℃; A and b for experience coefficient.
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