| 福建沿海地区花岗岩残积土工程特性探讨 |
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| 引用本文： | 杨茂长.福建沿海地区花岗岩残积土工程特性探讨[J].资源环境与工程,2010,24(1):41-43. |
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| 作者姓名： | 杨茂长 |
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| 作者单位： | 福建省地质工程勘察院,福建,福州,350002 |
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| 摘 要： | 花岗岩在各种风化力作用下会形成厚度不等的残积土,垂直与水平方向上形成较大差异,决定其物理力学性质、结构性、不均匀性,及具崩解软化的特征,使其强度发生较大的变化。明确其具有明显的垂直差异性,影响到其强度上的差异性。
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| 关 键 词： | 残积土 风化成因 工程特性 不均匀性 崩解软化 |
Discussion on Characteristics of the Residual Soil of Granite in Costal Areas of Fujian |
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| YANG Maochang.Discussion on Characteristics of the Residual Soil of Granite in Costal Areas of Fujian[J].Resources Environment & Engineering,2010,24(1):41-43. |
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| Authors: | YANG Maochang |
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| Affiliation: | Geo-engineering Investigation Institute of Fujian;Fuzhou;Fujian 350002 |
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| Abstract: | Under the various types of weathering action,the residual soil with different thickness can be formed from granite.Difference of vertical and horizontal directions determines physical and mechanical properties,structural property,nonuniformity and characteristics of disintegrative softening.The residual soil changes its intension greatly,and it has obvious vertical difference can effect difference of intension. |
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| Keywords: | residual soil weathering genesis engineering characteristics nonuniformity disintegrative softening |
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