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Hydrothermal Exploration Best Practices and Geothermal Knowledge Exchange on Openei.

↑ 1.0 1.1 Katherine Young,Timothy Reber,Kermit Witherbee.

These instruments can identify the signatures of some minerals such as framework silicates that may be related to hydrothermal activity. Another type of long wave heat sensor collects information at higher wavelengths of around 8 to 14 micrometers. Data is usually collected from one or two bands and is used to detect relatively warm areas at the surface such as hot springs, hot pools, hot rock/lava and snow melt. Typical imaging devices used to collect data in these wavelengths are Forward Looking Infrared (FLIR) cameras. One type collects information in wavelengths between 3.0 and 5.0 micrometers (these wavelengths are actually medium range infrared but are grouped with the LWIR type surveys). There are two types of long wave heat sensors used to collect geothermal data. Long wave infrared (LWIR) is a remote sensing technique that is also referred to as thermal imaging. These instruments can identify the signatures of some minerals such as framework silicates that may be related to hydrothermal activity.'`UNIQ-ref-00000001-QINU`'' cannot be used as a page name in this wiki. Data is usually collected from one or two bands and is used to detect relatively warm areas at the surface such as hot springs, hot pools, hot rock/lava and snow melt.'`UNIQ-ref-00000000-QINU`' Another type of long wave heat sensor collects information at higher wavelengths of around 8 to 14 micrometers.

'Long wave infrared (LWIR) is a remote sensing technique that is also referred to as thermal imaging.Mechanism responsible for intercalation of dimethyl sulfoxide in kaolinite: Molecular dynamics simulations. Shuai Zhang, Qinfu Liu, Hongfei Cheng, Feng Gao, Cun Liu, Brian J.Pore Structure Control of Expanded Dickite and Its Application as a Clay Coating Layer on Cross-Linked Nonwoven Fabrics for Lithium-Ion Batteries.

Yao Liu, Yinshan Jiang, Fangfei Li, Bing Xue, Xinwang Cao.

Deformation and failure processes of kaolinite under tension: Insights from molecular dynamics simulations.

Hua Yang, ManChao He, ChunSheng Lu, WeiLi Gong.

Thermodynamic Mechanism and Interfacial Structure of Kaolinite Intercalation and Surface Modification by Alkane Surfactants with Neutral and Ionic Head Groups. Shuai Zhang, Qinfu Liu, Hongfei Cheng, Feng Gao, Cun Liu, and Brian J.The results obtained can help develop appropriate protocol to intercalate and delaminate clay layers for clay-based applications and products.

The present study offers a direct view of the specific driving force involved in urea intercalation in kaolinite. The siloxane surfaces function as H-acceptors to facilitate the intercalation of urea. The interaction energy of urea with alumina surfaces was greater than that with siloxane surfaces, indicating that the alumina surface plays a primary role in the intercalation of kaolinite by urea. The calculated interaction energies of urea molecules with kaolinite alumina and siloxane surfaces suggest that the intercalation of urea within kaolinite interlayers is energetically favorable. Additionally, MD simulations further provided insight into the interaction energies of urea with the kaolinite interlayer environment. The H-bonds of urea formed with kaolinite surfaces calculated directly from molecular dynamics simulation was consistent with the infrared spectroscopic results. The amine group (−NH 2) of urea functioned as H-donors interacting with basal oxygens on siloxane surfaces and/or the oxygens of hydroxyl groups on alumina surfaces. The carbonyl group (−C═O) of urea acted as H-acceptors for the hydroxyl groups on alumina surfaces. Infrared spectroscopic results indicated the formation of hydrogen bonds between urea and siloxane/alumina surfaces of kaolinite. Intercalation of urea in kaolinite was investigated using infrared spectroscopy and molecular dynamics simulation.