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offline Mr Brazil from Oh Joan, I love you so... on 2006-12-31 01:33 [#02024382]
Points: 1970 Status: Lurker





?



 

offline Mr Brazil from Oh Joan, I love you so... on 2006-12-31 01:35 [#02024384]
Points: 1970 Status: Lurker



fireworks


 

offline pigster from melbs on 2006-12-31 01:35 [#02024385]
Points: 4480 Status: Lurker



???


 

offline pigster from melbs on 2006-12-31 01:40 [#02024386]
Points: 4480 Status: Lurker



... LOL


 

offline chr on 2006-12-31 02:52 [#02024420]
Points: 64 Status: Regular



looks more like a sea urchin gay pride parade



 

offline stefano_azevedo from Pindorama (Brazil) on 2006-12-31 03:01 [#02024426]
Points: 4396 Status: Regular



OMG SANTA EXPLODED


 

offline JAroen from the pineal gland on 2006-12-31 03:26 [#02024449]
Points: 16065 Status: Regular



#43 2,5-DIMETHOXY-4-(n)-PROPYLTHIOPHENETHYLAMINE

SYNTHESIS: To a solution of 3.4 g of KOH pellets in 50 mL
hot MeOH, there was added a mixture of 6.8 g
2,5-dimethoxythiophenol (see under the recipe for 2C-T-2 for
its preparation) and 7.4 g (n)-propylbromide dissolved in 20
mL MeOH. The reaction was exothermic, with the deposition of
white solids. This was heated on the steam bath for 0.5 h,
added to 800 mL H2O, additional aqueous NaOH added until the
pH was basic, and extracted with 3x75 mL CH2Cl2. The pooled
extracts were washed with dilute NaOH, and the solvent
removed under vacuum. The residue was 2,5-dimethoxyphenyl
(n)-propyl sulfide which was obtained as a pale yellow oil,
and which weighed 8.9 g. It had a light pleasant fruity
smell, and was sufficiently pure for use in the next
reaction without distillation.

A mixture of 14.4 g POCl3 and 13.4 g N-methylformanilide was
heated for 10 min on the steam bath. To this claret-colored
solution was added 8.9 g of 2,5-dimethoxyphenyl (n)-propyl
sulfide, and the mixture heated an additional 25 min on the
steam bath. This was then added to 800 mL of well-stirred
warm H2O (pre-heated to 55 °C) and the stirring continued
until the oily phase had completely solidified (about 15
minutes). The resulting brown sugar-like solids were removed
by filtration, and washed with additional H2O. After sucking
as dry as possible, they were dissolved in an equal weight
of boiling MeOH which, after cooling in an ice-bath,
deposited pale ivory colored crystals. After filtration,
modest washing with cold MeOH, and air drying to constant
weight, there was obtained 8.3 g of
2,5-dimethoxy-4-(n-propyl-thio)benzaldehyde with a mp of
73-76 °C. Recrystallization from 2.5 volumes of MeOH
provided a white analytical sample with mp 76-77 °C. The
NMR spectrum in CDCl3 was textbook perfect, with the two
aromatic protons showing singlet signals at 6.81 and 7.27
ppm, giving assurance that the assigned location of the
introduced aldehyde group was correct.


 

offline Ezkerraldean from the lowest common denominator (United Kingdom) on 2006-12-31 04:45 [#02024475]
Points: 5733 Status: Addict | Followup to JAroen: #02024449



i love IDM-techno-babble.

Microbial mat biotas dominated by cyanobacteria, are
commonly preserved in Meso- and Neoproterozoic carbonate
facies, the first well-documented case being the Bitter
Springs biota of central Australia (Schopf, 1968Go). Such
microfossils are preserved in three dimensions due to the
very early (i.e., prior to degradational collapse)
diagenetic emplacement of silica, from which point they
become more or less impervious to subsequent diagenetic, and
even low grade metamorphic alteration (Knoll, 1992Go). The
quality of preservation can be spectacular but,
unfortunately, the view is profoundly biased. The Bitter
Springs-type "taphonomic window" is limited to conspicuously
shallow-water/supratidal carbonate environments and is
conspicuously absent in the Phanerozoic. The reason lies in
the disjunct history of silica biogeochemistry. Prior to the
appearance of silica biomineralizers in the terminal
Proterozoic, surface waters of the oceans would have been
saturated with respect to silica, and supersaturated in
restricted peritidal settings (Maliva et al., 1989Go). These
restricted environments would also have been dominated by
prolific microbial mats which, as they decayed, served as
foci for the nucleation and precipitation of silica (Knoll,
1985Go). Such paleoenvironments were far from equable and,
with a few notable exceptions (e.g., Zhang et al., 1998Go;
Butterfield, 2000Go), tended to exclude eukaryotic
organisms. So despite its exceptional preservation, this
taphonomic mode fails to offer even a broad approximation of
paleodiversity. Moreover, the disappearance of Bitter
Springs type biotas at the end of the Proterozoic in no way
reflects biological extinction; rather, it is a taphonomic
signal induced by the evolution of silica-biomineralizing
sponges and consequent draw-down of marine silica
concentrations.


 

offline JAroen from the pineal gland on 2006-12-31 04:53 [#02024483]
Points: 16065 Status: Regular



will your diagenetic silica infusion make my pupils dilate?
DIDN'T THINK SO


 

offline JAroen from the pineal gland on 2006-12-31 04:57 [#02024484]
Points: 16065 Status: Regular | Followup to Ezkerraldean: #02024475



anyway is it talking about silicon based life or just stupid
bacteria remotely involved in silicon?


 


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