序号工程名称坝型及坝高岩性孔隙容重比重率2.422.692.432.492.462.442.522.2.52四川岷江鱼咀水电站(技施)侏罗系细粒砂岩侏罗系粉粒砂岩当地材料坝侏罗系中粗砂岩(25米)侏罗系粗粒砂岩侏罗系砂质页岩2.2582.572.692.722.682.702.702.692.722.732.732.6.309.3083498.043.306.97.07.473.345.614.12吸水率2.702.703.262.232.951.83饮和饮和干抗压湿抗压软化岩/岩吸水系数强度强度系数tgQ率0.0.0.97123559352079759931063805200-7000.670.670.981202123996811791044107980010250.860.0.820.870.780.800.570.85毛糙面抗剪0.630.551062113311137208007174900.860.40.960.550.740.810.680.610.710.710.490.520.620.630.600.650.690.600.700.35-0.45C0.250.150.200.010.040.100.140.190.100.450.300-0.450.620.600.160.181.761.6饮和抗剪砼/岩tgQC试验岩/岩条件建议值0.600.600.410.450.470.5-0.01-0.520.040.40-0.06-0.460.100.550.550.550.5-0.650.5-0.650.06C砼/岩建议tgQ0.650.651黄河盐锅峡(施工)白垩系砂质砾岩致密坚砼重力坝55硬米白垩系河口群紫红色砂(45)岩岩上粘土质粉砂岩砼流坝式重侏罗系重庆结砂岩中细力坝铁质胶结(35米)侏罗系重庆砂质粘土岩2四川龙溪河下硐(施工)3侏罗系砂岩中粒交错层四川龙溪溢流式重力透镜体多坝河下硐(侏罗系砂质土岩紫褐色技施)(6.7-8米)、钙质结42.66-2.68-1.8-2.622.734.152.66侏罗系中粒砂岩侏罗系细粒砂岩侏罗系粉粒砂岩侏罗系中粒砂岩侏罗系粗粒砂岩侏罗系砂质页岩2.652.662.682.722.732.722.743.532.863.132.92川岷紫平铺(修改初设)砼重力坝(68米)81米)平铺序号(修改初工程名称设)侏罗系细粒砂岩侏罗系粉粒砂岩(68米)侏罗系中粒砂岩坝型及坝高岩性81米)侏罗系粗粒砂岩侏罗系砂质页岩孔隙容重比重率2.342.572.622.702.702.722.604.813.88吸水率饮和饮和干抗压湿抗压软化岩/岩吸水系数强度强度系数tgQ率136657756775030031261931870226170.550.520.550.840.960.820.660.650.620.490.0.560.660.580.680.530.870.32C0.300.500.800.040.090.100.070.33砼/岩tgQC面抗剪岩/岩试验条件建议值C砼/岩建议tgQ6四川跳鱼坑(技施)四川渠河回九滩(初设)四川嘉陵江东西关寨(初设)土坝(30米)侏罗系中细粒长石石英砂岩侏罗系红色砂质粘土岩2.382.502.392.512.382.2.6711.502.7077.172.6911.602.722.712.757.412.56.593.727393310.60-0.620.430.620.450.600.030.1078侏罗系细中细粒砂岩重力溢流坝侏罗系砂质粘土岩(36米)交错层及斜层发育灰白色侏罗系砂岩厚15-19米重力溢流坝侏罗系砂质粘土堓或土坝(43.3米)岩相变化大,砂页岩互层3.902.53.662.848603809423162.28侏罗系统泥质砂岩和侏罗系狮子滩砂岩侏罗系大田沟砂岩侏罗系砂质粘土岩侏罗系粘土岩2.422.492.562.552.42四川岷江10偏密子(初设)
砼重力坝(87米)侏罗系统长石砂岩侏罗系砂砾岩侏罗系泥质粉砂岩侏罗系红色粘土岩及砂质粘土岩
2.462.682.602.672.692.702.712.725.569.56.514.355.605675396243702401028421945024511986750.760.780.720.660.500.630.610.400.550.340.420.780.760.060.060.090.100.120.250.100.900.729四川尤溪河狮子滩(施工)堆石坝(51米)tgQ为砂岩与下部粘土堓的抗剪值0.520.340.460.460.380.580.500.050.050.070.080.100.040.67序号四川岷江工程名称坝型及坝高侏罗系砂砾岩岩性砼重力坝10偏密子侏罗系泥质粉砂岩(87米)(初设)侏罗系红色粘土岩及砂质粘土岩孔隙容重比重率2.62.73吸水率饮和饮和干抗压湿抗压软化岩/岩吸水系数强度强度系数tgQ率793590135247512286268214240.170.7C0.170.0.15-0.120.260.190.220.20.10.130.120.040.090.160.070.590.590.2砼/岩tgQC试验岩/岩条件建议值0.520.36C0.070.2砼/岩建议tgQ0.24-0.342.592.752.472.698.32.832.20.420.630.620.21-0.57814902942232.372.6610.7四川清衣11江千佛岩侏罗系砂岩(新鲜)砼坝与岩地侏罗系砂岩(未风化)材料坝比较侏罗系砂质粘土岩(100米)侏罗系粘土岩侏罗系粘土岩2.522.736.172.442.736.732.362.732.67白垩系紫红色砂岩(轻风化)白垩系粘土质砂岩(轻风化)白垩系灰紫色石灰长石砂岩白垩系灰紫色砂岩(中等风化)白垩系砂紫砂质页岩(中等风化)白垩系灰紫色砂质页岩(轻风化)下白垩紫红色细粒石英长石砂岩白垩系紫红色细粒长石石英砂岩白垩系红色砾岩2.78.61.10.590.690.550.0.730.60.06-0.04-0.520.320.110.0.662.332.661.592.572.7.362.322.332.7153.591.9.4841.84.260.8516812.150.915736158635226204703423884920.50.40.590.6黄河八盘12峡(初设)砼重力坝(33.2米)6.220.725.070.822.50.70.680.0.40.630.490.570.420.550.420.550.60.590.90.160.670.222.612.332.472.572.362.572.715.762.032.6924.452.412.032.6924.452.412.512.729.551.41255255290106106175陕西圣河13大佛寺(初设)均质土(.4米)序号工程名称14 楚河 都1川嘉陵江合川坝型及坝高岩性孔隙容重比重率2.652.782.492.724.75吸水率0.661.2饮和饮和干抗压湿抗压软化岩/岩吸水系数强度强度系数tgQ率4424.0.244551630.370.52C0.28砼/岩tgQC试验岩/岩条件建议值C砼/岩建议tgQ土石混合坝白垩系砂质粘土岩土石坝或砼侏罗系砂质粘土岩坝 层 岩 石 物 理 力 学 指 标 表
C地质构造坝区为中生界凹陷盆地,坝坦无断层, 上坝址上游100米,下游400米处有二条横穿河谷断层,破碎带宽0.1-1.5米,倾角63°~85°。岸为砂质岩化碳向上游,在坝以下有风化破碎带,坝基及完整砂岩碎风化深,破碎带及夹泥多坝区有二组节理。坝基为砂岩,右坝肩为砂质粘土层,易风化,全厚30-40米,为单斜构造,无 皱断层。主付坝基为河床冲击层,基岩为砂质岩,倾向下游,倾角10°-20°,缓倾角节理发育,并有粘土充填,下游10-30米处有宽0.0-8-10米的12号断层穿过。0.2①糜 中粒砂岩,节理发育,有剪切力错动及挤压破碎,岩块0.2-1.0m层面夹有煤块。②砂质页岩夹 层粉粒砂及煤页岩,岩石破碎,节理发育,煤质页岩较新。③ 为破碎面较弱。砂岩中有四组裂隙,面岩中有三组。
C 中粒砂岩,节理发育,有剪切力错动及挤压破碎,岩块0.2-1.0m层面夹有煤块。
②砂质页岩夹 层粉粒砂及煤页岩,岩石破碎,节理发育,煤地质构造质页岩较新。③ 为破碎面较弱。砂岩中有四组裂隙,面岩中有三组。岩石走向平行坝轴,砂岩构造裂隙发育宽1-5mm,有泥。有二组节理,坝址岩层透水率、坝轴上下游均有小的正断层出现。层理近水平,节理有一组近与河流平行,有裂隙宽0.5-5cm,有岸坡剪力节理。岩相变化大,节理裂隙较发育,有二组宽0.1-0.5cm间距4-8m,有粘土风化物充填。除左述岩石外,沿有碳质页岩和淡水灰岩平行和垂直岩民支走向的节理发育,密度1.2-2.2条/米,裂隙率0.1%,坝区为一单斜构造的向上游,倾角17-22度。
C和淡水灰岩平行和垂直岩民支地质构造走向的节理发育,密度1.2-2.2条/米,裂隙率0.1%,坝区为一单斜构造的向上游,倾角17-22度。主要有二组裂隙,多闭合,岸边剪切节理发育间距2-5米,坝区为一背斜。坝区断层窄小,节理系剪性裂隙率0.96有%,分层 和同*行河道。岩层沿垂直及水平方向相交灰岩风化,软化,有层面 ,走向断层发育,岩层缓,为背斜,节理发育。C地质构造
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