An x-ray structural study of complexes of p-aminobenzoic acid with metals. X. The crystal structure of barium chloride p-aminobenzoate Ba(H2NC6H4COO)C1

1982 ◽  
Vol 23 (2) ◽  
pp. 267-269
Author(s):  
I. R. Amiraslanov ◽  
F. N. Musaev ◽  
Kh. S. Mamedov
Author(s):  
Selvam Karthik ◽  
Arunachalam Thirugnanasambandam ◽  
Pradeep Kumar Mandal ◽  
Namasivayam Gautham

The X-ray crystal structure of the DNA tetradecamer sequence d(CCGGGGTACCCCGG)2is reported at 1.4 Å resolution in the tetragonal space groupP41212. The sequence was designed to fold as a four-way junction. However, it forms an A-type double helix in the presence of barium chloride. The metal ion could not be identified in the electron-density map. The crystallographic asymmetric unit consists of one A-type double helix with 12 base pairs per turn, in contrast to 11 base pairs per turn for canonical A-DNA. A large number of solvent molecules have been identified in both the grooves of the duplex and around the backbone phosphate groups.


1991 ◽  
Vol 44 (8) ◽  
pp. 1145 ◽  
Author(s):  
MF Mackay ◽  
M Campbell ◽  
MJ Mcleish

The title compound formed the major component in a rearrangement of an analogue of 4-amino-4-deoxychorismic acid (1), an intermediate in the chorismate-p-aminobenzoic acid biotransformation. X-Ray crystallographic analysis has defined the relative stereochemistry at the four chiral centres in the tricyclic molecule.


1997 ◽  
Vol 12 (2) ◽  
pp. 76-80 ◽  
Author(s):  
A. El-Yacoubi ◽  
R. Brochu ◽  
A. Serghini ◽  
M. Louër ◽  
M. Alami Talbi ◽  
...  

A new mixed lead thorium phosphate, Pb0.5Th2(PO4)3, has been isolated in the system PbO–ThO2–P2O5. Its crystal structure (monoclinic symmetry, a=17.459(1) Å, b=6.8451(4) Å, c=8.1438(5) Å, β=101.247(5)°, space group C2/c) has been determined from conventional monochromatic X-ray powder diffraction data. The structure is related to the MITh2(PO4)3 structure type. Lead atoms are located in the channels parallel to the c axis, out of the twofold axis for 0.97 Å, and are statistically distributed on a quarter of crystallographic positions. The thermal stability of this material is greater than that of the monazite-type compound PbTh(PO4)2.


1980 ◽  
Vol 21 (3) ◽  
pp. 352-355 ◽  
Author(s):  
I. A. Baidina ◽  
N. V. Podberezskaya ◽  
S. V. Borisov ◽  
V. I. Alekseev ◽  
T. N. Martynova ◽  
...  

1982 ◽  
Vol 23 (3) ◽  
pp. 422-431 ◽  
Author(s):  
N. V. Podberezskaya ◽  
S. A. Magarill ◽  
I. A. Baidina ◽  
S. V. Borisov ◽  
L. �. Gorsh ◽  
...  

2000 ◽  
Vol 64 (5) ◽  
pp. 879-884 ◽  
Author(s):  
M. Pasero ◽  
D. Vacchiano

AbstractThe crystal structure of the rare secondary lead mineral georgiadesite has been solved from single-crystal X-ray diffraction data (R = 0.071). The structure can be visualized in terms of alternating puckered (100) layers of [Pbϕ6] octahedra and [Pbϕ8] bicapped trigonal prisms (ϕ = generic anion). Lead also occurs in irregular, lopsided polyhedra. This structural study shows unambiguously that arsenic occurs as As3+ and not as As5+. The chemical formula of georgiadesite has therefore been revised, on structural grounds, to Pb4(AsO3)Cl4(OH).


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