X-Ray Diffraction Table

X-Ray Diffraction Table

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Minerals Arranged by X-Ray Powder Diffraction

See Help on X-Ray Diffraction.

Powder X-ray Diffraction (XRD) is one of the primary techniques used by mineralogists and solid state chemists to examine the physico-chemical make-up of unknown materials. This data is represented in a collection of single-phase X-ray powder diffraction patterns for the three most intense D values in the form of tables of interplanar spacings (D), relative intensities (I/Io), mineral name and chemical formulae

The XRD technique takes a sample of the material and places a powdered sample in a holder, then the sample is illuminated with x-rays of a fixed wave-length and the intensity of the reflected radiation is recorded using a goniometer. This data is then analyzed for the reflection angle to calculate the inter-atomic spacing (D value in Angstrom units - 10-8 cm). The intensity(I) is measured to discriminate (using I ratios) the various D spacings and the results are compared to this table to identify possible matches. Note: 2 theta (Θ) angle calculated from the Bragg Equation, 2 Θ = 2(arcsin(n λ/(2d)) where n=1;

For more information about this technique, see X-Ray Analysis of a Solid or take an internet course at Birkbeck College On-line Courses.  Many thanks to Frederic Biret for these data.

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Listing of 26 Records Sorted by D1 using 1.54056 - CuKa1 for 2θ WHERE (d1 > 1.5092 AND d1 < 1.5708)
D1
Å (2θ)
I1
%)
D2
Å (2θ)
I2
(%)
D3
Å (2θ)
I3
(%)
Mineral Formula
1.511(61.30) 100 2.600(34.47) 90 5.200(17.04) 85 Takeuchiite Mg2Mn+++O2(BO3)
1.516(61.07) 100 2.163(41.72) 100 3.190(27.95) 100 Babefphite BaBe(PO4)(F,O)
1.516(61.07) 100 3.190(27.95) 100 2.163(41.72) 100 Babefphite BaBe(PO4)(F,O)
1.519(60.94) 100 2.600(34.47) 100 4.520(19.62) 80 Chromphyllite (K,Ba)(Cr,Al)2[AlSi3O10](OH,F)2
1.520(60.90) 100 15.400(5.73) 100 4.560(19.45) 100 Nontronite Na0.3Fe+++2(Si,Al)4O10(OH)2•n(H2O)
1.520(60.90) 100 4.560(19.45) 100 15.400(5.73) 100 Nontronite Na0.3Fe+++2(Si,Al)4O10(OH)2•n(H2O)
1.522(60.81) 100 2.410(37.28) 100 3.360(26.51) 90 Shirokshinite K(NaMg2)Si4O10F2
1.530(60.46)
-
2.610(34.33)
-
3.910(22.72)
-
Kurumsakite (Zn,Ni,Cu)8Al8V2Si5O35•27(H2O) (?)
1.530(60.46) 100 4.580(19.36) 100 15.800(5.59) 80 Hectorite Na0,3(Mg,Li)3Si4O10(OH)2
1.539(60.07) 100 1.804(50.55) 100 2.940(30.38) 100 Tazheranite CaTiZr2O8
1.539(60.07) 100 2.940(30.38) 100 1.804(50.55) 100 Tazheranite CaTiZr2O8
1.540(60.02) 100 2.660(33.67) 60 2.350(38.27) 60 Mcgovernite Mn9Mg4Zn2As2Si2O17(OH)14
1.540(60.02) 100 15.400(5.73) 100 2.670(33.54) 100 Sauconite Na0,3Zn3(Si,Al)4O10(OH)2•4(H2O)
1.540(60.02) 100 4.360(20.35) 100 3.590(24.78) 100 Neotocite (Mn,Fe++)SiO3•(H2O) (?)
1.540(60.02) 100 3.590(24.78) 100 4.360(20.35) 100 Neotocite (Mn,Fe++)SiO3•(H2O) (?)
1.540(60.02) 100 2.670(33.54) 100 15.400(5.73) 100 Sauconite Na0,3Zn3(Si,Al)4O10(OH)2•4(H2O)
1.540(60.02) 100 2.580(34.74) 100 2.880(31.03) 60 Pyrope Mg3Al2(SiO4)3
1.540(60.02) 100 2.350(38.27) 60 2.660(33.67) 60 Mcgovernite Mn9Mg4Zn2As2Si2O17(OH)14
1.540(60.02) 100 2.580(34.74) 100 2.880(31.03) 60 Majorite Mg3(Fe,Al,Si)2(SiO4)3
1.544(59.85) 100 2.556(35.08) 100 2.992(29.84) 60 Glagolevite NaMg6[Si3AlO10](OH,O)8•H2O
1.544(59.85) 100 2.992(29.84) 100 2.597(34.51) 60 Glagolevite NaMg6[Si3AlO10](OH,O)8•H2O
1.548(59.68) 100 1.813(50.28) 100 2.940(30.38) 100 Lewisite (Ca,Fe++,Na)2(Sb,Ti)2O7
1.548(59.68) 100 2.940(30.38) 100 1.813(50.28) 100 Lewisite (Ca,Fe++,Na)2(Sb,Ti)2O7
1.550(59.60) 100 2.522(35.57) 100 1.805(50.52) 92 Sabelliite Cu2Zn(As,Sb)O4(OH)3
1.552(59.51) 100 1.818(50.14) 100 2.950(30.27) 100 Uranmicrolite (U,Ca)2(Ta,Nb)2O6(OH)
1.552(59.51) 100 2.950(30.27) 100 1.818(50.14) 100 Uranmicrolite (U,Ca)2(Ta,Nb)2O6(OH)

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