Sensitivity of Clay Suspension Rheological Properties to pH, Temperature, Salinity, and Smectite‐Quartz Ratio

Kameda Jun; Morisaki Tomonori

摘要

Abstract > Understanding the rheological properties of clay suspensions is critical to assessing the behavior of sediment gravity flows such as debris flow or turbidity current. We conducted rheological measurements of composite smectite‐quartz suspensions at a temperature of 7°C and a salt concentration of 0.6? <fi>M</fi> . This is representative of smectite‐bearing sediments under conditions on the seafloor. The flow curves obtained were fitted by the Bingham fluid model, from which we determined the Bingham yield stress and dynamic viscosity of each suspension. At a constant smectite‐quartz mixing ratio, the yield stress and the dynamic viscosity tend to increase as the solid/water ratio of the suspension is increased. In the case of a constant solid/water ratio, these values increase with increasing smectite content in the smectite‐quartz mixture. Additional experiments exploring differing physicochemical conditions (pH?1.0–9.0; temperature 2–30°C; and electrolyte (NaCl) concentration 0.2–0.6? <fi>M</fi> ) revealed that the influence of temperature is negligible, while pH moderately affects the rheology of the suspension. More significantly, the electrolyte concentration greatly affects the flow behavior. These variations can be explained by direct and/or indirect (double‐layer) interactions between smectite‐smectite particles as well as between smectite‐quartz particles in the suspension. Although smectite is known as a frictionally weak material, our experimental results suggest that its occurrence can reduce the likelihood that slope failure initiates. Furthermore, smectite can effectively suppress the spreading distance once the slope has failed. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><Abstract Type =“Main”XML：Lang =“en”> <标题类型=“main”>抽象</标题> >了解粘土悬浮液的流变性质对于评估沉积物重力流动的行为至关重要碎屑流量或浊度电流。我们在7℃的温度和0.6的盐浓度下进行复合蒙脱石 - 石英悬浮液的流变测量。 <fi> m </ fi>。这是在海底的条件下掩护沉积物的代表。所获得的流动曲线由弯曲流体模型装配，我们确定了每种悬浮液的弯曲屈服应力和动态粘度。在恒定的蒙脱石 - 石英混合比中，随着悬浮液的固体/水比增加，屈服应力和动态粘度趋于增加。在恒定的固体/水比的情况下，这些值随着蒙脱石 - 石英混合物中的蒙脱石含量增加而增加。另外的实验探索不同的物理化学条件（pH？1.0-9.0;温度2-30°C;电解质（NaCl）浓度0.2-0.6？<Fi> m </ fi>）显示温度的影响忽略不计，而pH中度影响悬浮液的流变学。更显着，电解质浓度大大影响了流动行为。这些变化可以通过透析岩 - 蒙脱石颗粒之间的直接和/或间接（双层）相互作用来解释，以及悬浮液中的蒙脱石 - 石英颗粒之间。虽然蒙脱石被称为摩擦弱材料，但我们的实验结果表明其发生可以降低斜坡失效引发的可能性。此外，一旦斜坡发生故障，蒙脱土就能有效地抑制扩散距离。 </ p> </ abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-23539/'>《Geophysical Research Letters》</a> <b style="margin: 0 2px;">|</b><span>2017年第19期</span><b style="margin: 0 2px;">|</b><span>共7页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kameda Jun&option=202" target="_blank" rel="nofollow">Kameda Jun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Morisaki Tomonori&option=202" target="_blank" rel="nofollow">Morisaki Tomonori;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Earth and Planetary System Science Graduate School of ScienceHokkaido UniversitySapporo Japan;</p> <p>Earth and Planetary System Science Graduate School of ScienceHokkaido UniversitySapporo Japan;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/163.html" title="地球物理学">地球物理学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=smectite suspension&option=203" rel="nofollow">smectite suspension;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rheology&option=203" rel="nofollow">rheology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sediment gravity flow&option=203" rel="nofollow">sediment gravity flow;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=runout distance&option=203" rel="nofollow">runout distance;</a> </p> <div class="translation"> 机译：壁悬浮液;流变学;沉积物重力流动;跳动距离; 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