首页> 外文会议>WM '99 conference >CONE PERMEAMETER? – IN-SITU PERMEABILITY MEASUREMENTS WITH DIRECT PUSH TECHNIQUES
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CONE PERMEAMETER? – IN-SITU PERMEABILITY MEASUREMENTS WITH DIRECT PUSH TECHNIQUES

机译:锥度? –采用直接推动技术进行现场渗透率测量

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Soil permeability, which defines the magnitude of fluid flow (gas or liquid) underimposed pressure gradients, is one of the most important hydrologic parameters tomeasure when predicting fluid or contaminant movement in the subsurface, designingenvironmental remediation systems, or simply characterizing a geologic site. Scienceand Engineering Associates, Inc. (SEA), has developed the Cone Permeameter?, a conepenetrometer technology that measures the in-situ air permeability or hydraulicconductivity in unconsolidated media. The cone permeameter rod incorporates awell-defined injection zone and multiple pressure ports placed at discrete locations fromthe injection zone. A permeability value is obtain by injecting a known flowrate of air orwater, measuring the pressure response along the permeameter rod, and then applying aone-dimensional, spherical, steady-state Darcy flow model to the measured injection rateand pressure profile. Near to the injection point the pressure field is distorted by acombination of the cylindrical injection zone and the compacted soil near the rod surface.A fundamental premise of the measurement is that, as the distance from the injectionpoint is increased, the resulting pressure distribution will become spherical. This methodmeasures the pressure gradient far enough from the injection point to avoid the distortedfield.The Cone Permeameter? measurement system has the following benefits overexisting in-situ permeability methods:1. All the advantages of direct push: minimal waste, risk reduction, fast emplacement,low unit measurement cost2. 3 to 10 minute measurement time per elevation3. Rapid mobilization and minimal site disturbance4. Complements standard CPT geophysical measurements5. Higher spatial resolution possible than borehole techniques (<10 vs. 50+ cm.)6. Potentially more accurate and quantified permeability measurements7. Compared to the pore pressure dissipation technique, which can only measure in lowpermeability water saturated media, the Cone PermeameterTM system can measurefive orders of magnitude in both saturated and unsaturated environmentsThe initial research and feasibility assessment of this system was completed inearly 1997 as the first phase of a contract supported by the DOE Characterization,
机译:土壤渗透率定义了施加在压力梯度下的流体(气体或液体)的大小,是预测地下流体或污染物运移,设计环境修复系统或简单描述地质部位时要测量的最重要的水文参数之一。 Science and Engineering Associates,Inc.(SEA)已开发出Cone Permeameter ?,这是一种锥形渗透仪技术,用于测量非固结介质中的原位空气渗透率或水力传导率。锥形渗透计杆包含一个定义明确的注入区和多个压力端口,这些压力端口位于与注入区不同的位置。通过注入已知的空气或水流量,测量沿渗透计杆的压力响应,然后将一维,球形,稳态达西流动模型应用于所测得的注入速率和压力曲线,可获得渗透率值。靠近注入点时,圆柱注入区域和靠近杆表面的压实土壤的结合使压力场变形。测量的基本前提是,随着距注入点距离的增加,最终的压力分布将变为球形。该方法测量距注入点足够远的压力梯度,从而避免场失真。测量系统与现存的原位渗透率方法相比具有以下优点:1。直接推送的所有优点:浪费最少,风险降低,安装速度快,单位测量成本低2。每个高程3至10分钟的测量时间3。快速动员和最小的现场干扰4。补充标准CPT地球物理测量结果5。可能比钻孔技术具有更高的空间分辨率(<10 vs. 50+ cm。)6。潜在更准确和量化的渗透率测量7。与只能在低渗透水饱和介质中进行测量的孔隙压力耗散技术相比,Cone PermeameterTM系统可以在饱和和非饱和环境中测量五个数量级。该系统的初步研究和可行性评估于1997年初完成,是第一阶段。 DOE表征支持的合同,

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  • 来源
    《WM '99 conference》|1999年|p.1-9|共9页
  • 会议地点 Tucson, AZ(US)
  • 作者单位

    Science and Engineering Associates3205 Richards Lane Suite A Santa Fe NM 87505Phone: (505) 424-6955Fax: (505) 424-6956eMail: blowry@seabase.com;

    Science and Engineering Associates3205 Richards Lane Suite A Santa Fe NM 87505Phone: (505) 424-6955Fax: (505) 424-6956;

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