In particular, we will show here that any Stability Zone actually has a second boundary, restricting a larger region with a certain behavior of conductivity. Besides that, we shall discuss here general questions of complexity of the angular diagrams for the conductivity and propose a theoretical ...
Stability of excavations in the zone influenced by cleaning operationsSimple Lie groupsControllabilityInvariant vector fieldsRoot systemsAbstract Without Abstractdoi:10.1007/BF02499776Vasiliy Dmitrievich BaryshnikovV. I. MashukovK. V. PirlyaKluwer Academic Publishers-Plenum PublishersSoviet Mining Science...
it can be extrapolated that shelf life of Rasayana Churna is 25.12 months (2.09 years) for countries which comes under climatic zone I & II and 16.60 months (1.38 years) for countries which comes under climatic zone III & IV. Real time stability data of Rasayana Churna showed very good ...
ICH Q1F Guideline - Stability Data Package for Registration in Climatic Zones III and IV 1.6 ICH Q1F Guideline Stability Data Package for Registration in Climatic Zones III and IV Step 4 in the ICH process Comments for its application ICHQ1F C 59 ...
ICHQ1FC59 1.6 ICHQ1FGuideline StabilityDataPackagefor Registrationin ClimaticZonesIIIandIV Step4intheICHprocess Commentsforitsapplication ICHQ1FC60 1.GeneralConsideration Definitionandstorageconditionsforthefourclimaticzones ClimaticzoneDefinitionStoragecondition I II III IV temperateclimate subtropicaland Mediterr...
Further work by the ICH Stability Working Group led to the idea of a single long-term stability condition for Zone IV countries which would also serve as an intermediate condition/alternative long-term condition for Zone II countries. Their proposal to use 30...
In addition, ARL2 is localized at the centrosome in cell lines where it is proposed to act as a microtubule regulator in an ARL2BP-independent manner14. These data suggest that ARL2 may play a role in OS formation by regulating tubulin or ARL2BP at photoreceptor cilium. The purpose of ...
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Transpiration leads to desaturation of the soil which again leads to a lowering of the water table and suction development in the unsaturated zone (Zhu et al. 2018). The transpiration-induced soil suction acts as a reinforcement on slope stability and can be included in the Mohr-Coulomb failure...
For Y zeolites, the low-temperature zone (100–250 °C) of the desorption peak is ascribed to weak acid sites, the high-temperature zone (400–600 °C) corresponds to strong acid sites, and the temperature zone between weak acid sites and strong acid sites (250–400 °C) belongs...