Ultra-Violet/Electron Beam Detoxification of Nitroglycerin/Propylene Glycol Dinrate Waste Water, Phase 1

1994 ◽  
Author(s):  
DAMILIC CORP ROCKVILLE MD
Author(s):  
Sumio Iijima ◽  
Toshinari Ichihashi

Formation of twins in Or-BYCO crystals was studied by transforming them to T-phase by electron beam irradiation in the microscope. It is known that during the transformation the crystals developed twinning (STW), Ortho-II phase (1×2 superstructure), tweed structure. These structures occur in that order by the irradiation and the structural changes are caused by oxygen deficiency and oxygen atoms ordering. This work is aimed at elucidation of oxygen atom ordering by examining the structural evolution in terms of morphologies of the twins.Atypical evolution of an Or-BYCO crystal is shown in a series of micrographs in Figs. 1 to 5. As-grown twin (FTW) boundaries have a characteristic lens shape extending in the < 110> direction and terminate at a twin boundary in horizontal direction (Fig.1). These boundaries don't accompany strain contrast which is developed in the crystal after a brief irradiation (Fig.2). The strain contrasts, which are differentiated easily from the thickness contrast, appear parallel to the boundaries and change slowly across the boundaries.


Molecules ◽  
2014 ◽  
Vol 19 (8) ◽  
pp. 11860-11882 ◽  
Author(s):  
Elham Jahangiri ◽  
Senta Reichelt ◽  
Isabell Thomas ◽  
Kristin Hausmann ◽  
Dietmar Schlosser ◽  
...  

Polymer ◽  
1989 ◽  
Vol 30 (6) ◽  
pp. 1091-1098 ◽  
Author(s):  
J. Woods ◽  
J. Guthrie ◽  
J. Rooney ◽  
L. Kelly ◽  
A. Doyle ◽  
...  

2021 ◽  
Vol 288 (1944) ◽  
pp. 20202263
Author(s):  
M. Gabriela Mángano ◽  
Luis A. Buatois ◽  
Beatriz G. Waisfeld ◽  
Diego F. Muñoz ◽  
N. Emilio Vaccari ◽  
...  

Trilobites, key components of early Palaeozoic communities, are considered to have been invariably fully marine. Through the integration of ichnological, palaeobiological, and sedimentological datasets within a sequence-stratigraphical framework, we challenge this assumption. Here, we report uncontroversial trace and body fossil evidence of their presence in brackish-water settings. Our approach allows tracking of some trilobite groups foraying into tide-dominated estuaries. These trilobites were tolerant to salinity stress and able to make use of the ecological advantages offered by marginal-marine environments migrating up-estuary, following salt wedges either reflecting amphidromy or as euryhaline marine wanderers. Our data indicate two attempts of landward exploration via brackish water: phase 1 in which the outer portion of estuaries were colonized by olenids (Furongian–early late Tremadocian) and phase 2 involving exploration of the inner to middle estuarine zones by asaphids (Dapingian–Darriwilian). This study indicates that tolerance to salinity stress arose independently among different trilobite groups.


1988 ◽  
Author(s):  
W M. Kelly ◽  
A Doyle ◽  
E. Noonan ◽  
J Woods ◽  
J Rooney
Keyword(s):  

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