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Testing of explosives mixed with clay to determine maximum explosive content of non-reactive mixtures

机译：测试与粘土混合的炸药，以确定非反应性混合物的最大爆炸含量

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Garza, R; Green, L; Maienschein, J; Pruneda, C;
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年度 1998
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机译：基于沥青砂浆试验确定疲劳性能良好的石基沥青混合料最大RAP含量的反算方法
2. Explosive Mixtures for Explosive Welding of Thin Foils: Part 2. RDX-Baking Soda Mixtures [J] . Leonid A. Andreevskikh, Yury P. Dendenkov, Oleg B. Drennov Propellants, Explosives, Pyrotechnics . 2011,第5期

机译：薄箔爆炸焊接用炸药混合物：第2部分。RDX小苏打混合物
3. Maximum Explosive Pressure and Temperature of Vapor-Air Mixtures [J] . N. I. Akinin, I. V. Babaitsev, V. K. Kriventsova Coke and chemistry . 2011,第8期

机译：蒸气-空气混合物的最大爆炸压力和温度
4. Determining the incendivity of electrostatic discharges without explosive gas mixtures [C] . von Pidoll, U., Brzostek, Industry Applications Conference, 2002. 37th IAS Annual Meeting. Conference Record of the . 2002

机译：测定没有爆炸性气体混合物的静电放电的可能性
5. The viscosity of dacitic liquids measured at conditions relevant to explosive arc volcanism: Determining the influence of temperature, silicate composition, and dissolved volatile content. [D] . Hellwig, Bridget M. 2006

机译：在与爆炸弧火山作用有关的条件下测得的daictic液体的粘度：确定温度，硅酸盐组成和溶解的挥发物含量的影响。
6. Application of a catalytic combustion sensor (Pellistor) for the monitoring of the explosiveness of a hydrogen-air mixture in the upper explosive limit range [O] . M. Krawczyk, J. Namiesnik 2003

机译：催化燃烧传感器（Pellistor）在爆炸上限内用于监测氢气混合物的爆炸性的应用
7. The oceans mediate the response of global climate to natural and anthropogenic forcings. Yet for the past 2,000 years — a key interval for understanding the present and future climate response to these forcings — global sea surface temperature changes and the underlying driving mechanisms are poorly constrained. Here we present a global synthesis of sea surface temperatures for the Common Era (ce) derived from 57 individual marine reconstructions that meet strict quality control criteria. We observe a cooling trend from 1 to 1800 ce that is robust against explicit tests for potential biases in the reconstructions. Between 801 and 1800 ce, the surface cooling trend is qualitatively consistent with an independent synthesis of terrestrial temperature reconstructions, and with a sea surface temperature composite derived from an ensemble of climate model simulations using best estimates of past external radiative forcings. Climate simulations using single and cumulative forcings suggest that the ocean surface cooling trend from 801 to 1800 ce is not primarily a response to orbital forcing but arises from a high frequency of explosive volcanism. Our results show that repeated clusters of volcanic eruptions can induce a net negative radiative forcing that results in a centennial and global scale cooling trend via a decline in mixed-layer oceanic heat content. [O] . McGregor, Helen V., Evans, Michael N., Goosse, Hugues, 2015

机译：海洋调节了全球气候对自然和人为强迫的响应。然而，在过去的2,000年中（这是了解当前和未来气候对这些强迫的响应的关键间隔），全球海表温度变化及其潜在的驱动机制受到的约束很有限。在这里，我们提出了一个共同的时期（ce）的全球海面温度的全球综合，该综合来自57个符合严格质量控制标准的海洋重建项目。我们观察到从1到1800 ce的冷却趋势，对于显式测试重建中潜在的偏倚而言，该趋势很稳健。在801至1800 ce之间，表面降温趋势在质量上与地面温度重建的独立合成以及从使用过去外部辐射强迫的最佳估计的气候模型模拟集合推导出的海面温度合成在质量上是一致的。使用单一和累积强迫的气候模拟表明，从801到1800 ce的海洋表面冷却趋势主要不是对轨道强迫的反应，而是爆炸性火山爆发的频繁发生。我们的结果表明，火山喷发的反复簇可引起净的负辐射强迫，这会导致混合层海洋热量降低而导致百年和全球规模的降温趋势。

Testing of explosives mixed with clay to determine maximum explosive content of non-reactive mixtures

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