title 政木, 清孝; 磯村尚子; 山本広美 沖縄工業高等専...
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Title 海洋生物の生成する炭酸カルシウムのX線回折測定
Author(s) 政木, 清孝; 磯村尚子; 山本広美
Citation 沖縄工業高等専門学校紀要 = Bulletin of Okinawa NationalCollege of Technology(9): 1-12
Issue Date 2015-03
URL http://hdl.handle.net/20.500.12001/18711
Rights 沖縄工業高等専門学校
X-Ray diffraction method
XRD
1 400mm Acropora
intermedia
1 2 a 5
MC110 2 b
2~3mm
3 Mizuhopecten yessoensis
(a) Sampling position (b)Shape of sample
Fig.1 The skeleton of Acropora intermedia Fig.2 Detail of XRD measurement sample
2~3mm
15mm
2 Bulletin of Okinawa National College of Technology, No.9 (2015)
5
4 a
15mm No.1 10mm 5mm×5mm
A-2 A-3
C-2 C-3
X 5 X XRD-6100 Cu
50kV 35mA X Ni
2mm 2 0.02 deg 1.0
deg/min 10 80 deg 6
X
PatView K 2
American Mineralogist Crystal Structure Database AMCSD
(a) Left shell (b) Right shell
Fig.3 The Shells of Mizuhopecten yessoensis
(a) Left shell (b) Right shell
Fig.4 Sampling position and shape of sample
Inside Inside Outside Outside
The site for attachment of adductor muscle
3沖縄高専紀要 第 9号(2015)
Fig.5 XRD measurement equipment. Fig.6 Example of sample setting
X 7 AMCSD
100%
7
Position 1 Position 2
42.94 deg
45.90 deg
X
48 deg
48.35 deg
48.51 deg Position 1 Position 2
Position 3 Position 2
42.06 deg 62.70 deg 75.16 deg [A]
Position 2
Position 5
3
Position 4 [B]
[A]
42.94 deg 63.39 deg 76.85 deg
[A]
Coral
Shell
4 Bulletin of Okinawa National College of Technology, No.9 (2015)
Fig.7 XRD profiles of Acropora intermedia as shown in Fig.2(a).
0.5
1.0
1.5
2.0[ 104]In
tens
ity /
cps position 1
20 30 40 50 60 70 80
0.5
1.0
1.5
2.0[ 104]
2 / deg
Inte
nsity
/ cp
s position 5
[ A ][ A ] [ A ]
[ A ]
[ A ]
[ A ]
[ B ]
[ B ]
[ B ]
(1 1 1)
(2 2 0)
(2 2 1)
(0 4 1) (2 0 2)
(1 5 1)
(2 2 0)
(2 0 4) (4 0 0)
0.5
1.0
1.5
2.0[ 104]
Inte
nsity
/ cp
s position 2
0.5
1.0
1.5
2.0[ 104]
Inte
nsity
/ cp
s position 3
20 30 40 50 60 70 80
0.5
1.0
1.5
2.0[ 104]
Inte
nsity
/ cp
s position 4
5沖縄高専紀要 第 9号(2015)
X 8
0~10000cps AMCSD
A-2 A-3
A-1 29.42 deg
47.54 deg
77 deg
72.95 deg
58deg
AMCSD
A-2 A-3
31.17 deg
58deg A-4
A-5 37 deg 77 deg
B
58 deg
47 deg
A B 77 deg
A-1 B-1 Unknown peak
X 9 C-2 C-3
A-2 A-3
31.17 deg
D B
47 deg
C D
77 deg C-1 D-1
42 deg C-1 D-1 Unknown peak
6 Bulletin of Okinawa National College of Technology, No.9 (2015)
Fig.8 XRD profiles of Mizuhopecten yessoensis (Left shell)
20 30 40 50 60 70 800
5000
10000
Inte
nsity
/ cp
s B-220 30 40 50 60 70 800
5000
10000
Inte
nsity
/ cp
s B-320 30 40 0 60 0 800
5000
10000
Inte
nsity
/ cp
s B-420 30 40 50 60 70 800
5000
10000
Inte
nsity
/ cp
s B-5
20 30 40 50 60 70 800
0
0A-2
0
0
0A-3
0
0
0A-4
20 30 40 50 60 70 800
0
0A-5
20 30 40 50 60 70 800
5000
10000
2� / deg
Inte
nsity
/ cp
s A-1
20 30 40 50 60 70 800
5000
10000
2� / deg
Inte
nsity
/ cp
s B-1
Aragonite
Calcite
Aragonite
Calcite
C(104) C(018)
A(002)
C C C A
A
A A C C C A
A
C A
C C
C(018) C(116)
C(116)
Unknown peak Unknown peak
A
7沖縄高専紀要 第 9号(2015)
Fig.9 XRD profiles of Mizuhopecten yessoensis (Right shell)
0
0
0D-2
0
0
0D-3
0
0D-4
20 30 40 0 60 0 800
0
0D-5
20 30 40 50 60 70 800
5000
10000
2� / deg
Inte
nsity
/ cp
s D-1
0
5000
10000
Inte
nsity
/ cp
s C-5
20 30 40 0 60 0 800
5000
10000
Inte
nsity
/ cp
s C-4
20 30 40 0 60 0 800
5000
10000
Inte
nsity
/ cp
s C-3
0
5000
10000
Inte
nsity
/ cp
s C-2
20 30 40 50 60 70 800
5000
10000
2� / deg
Inte
nsity
/ cp
s C-1
Aragonite
Calcite
Aragonite
Calcite
C(104) C(018)
A(002)
A
A
C
C(018) C(116) C(116) Unknown peak
Unknown peak C(104)
Unknown peak Unknown peak
8 Bulletin of Okinawa National College of Technology, No.9 (2015)
X
7 [A]
[B]
Unknown peak
A-1 B-1 C-1 D-1
nsind2 orsinnd2 (1)
d X n
d
CaCO3
Ca
Ca
Mg Ca Mg mol Mg
29.42 deg 7
30 deg
Mg
Mg 12 Ca 20
Ca Mg
Sr Sr Ca
Ca
Sr
9沖縄高専紀要 第 9号(2015)
AMCSD Sr
42.97 deg
42.94 deg AMCSD Strontianite (SrCO3)
41.55 deg
Position 5 XRD
42 deg 77 deg
Sr
Strontianite (SrCO3)
Position 4
Strontianite (SrCO3) Ca Sr Aragonite
X Energy
dispersive X-ray spectrometry EDX
Acropora intermedia X
Mizuhopecten yessoensis X
1
2
3
21 5
177 188 2012
10 Bulletin of Okinawa National College of Technology, No.9 (2015)
(Scleractinia) : 1. 66
8C 14 1963
JGL 4 4 6 7 2008
M&M'14 CD-ROM No.GS23, 1 4 2014 .
114 117 2013
21 5 159 175 2012
http://mukiken.eng.niigata-u.ac.jp/chemsoft/x-raysoft/PatViewHelp.html
http://rruff.geo.arizona.edu/AMS/amcsd.php
http://rruff.geo.arizona.edu/AMS/amcsd.php (Dal Negro A, Ungaretti L, American Mineralogist 56,768-772
(1971))
http://rruff.geo.arizona.edu/AMS/amcsd.php (Graf D L, American Mineralogist 46, 1283-1316 (1961))
W.D. [1] 62 67 2002
53 3
162 165 (1999)
Higuchi T Fujimura H Yuyama I Harii S Agostini S et al. Biotic Control of Skeletal Growth by
Scleractinian Corals in Aragonite Calcite Seas PLoSONE 9(3) e91021. doi:10.1371 2014
Anja Reitz Gert J. de Lange Abundant Sr-rich aragonite in eastern Mediterranean sapropel S1: Diagenetic
vs. detrital/biogenic origin Palaeogeography, Palaeoclimatology, Palaeoecology 235 135 148 2006
N. Allison A.A. Finch S.R. Sutton M. Newville Strontium heterogeneity and speciation in coral
aragonite: implications for the strontium paleothermometer Geochimica et Cosmochimica Acta 65 16 2669
2676 2001
Michael Holcomb Anne L. Cohen Rinat I. Gabitov Jeffrey L. Hutter Compositional and morphological
features of aragonite precipitated experimentally from seawater and biogenically by corals Geochimica et
Cosmochimica Acta 73 14-15 4166 4179 2009
http://rruff.geo.arizona.edu/AMS/amcsd.php (Ye Y, Smyth J R, Boni P, American Mineralogist 97, 707-712
(2012))
http://rruff.geo.arizona.edu/AMS/amcsd.php (de Villiers J P R, American Mineralogist 56, 758-767 (1971))
11沖縄高専紀要 第 9号(2015)
X-Ray diffraction measurement of marine-derived calcium carbonate
Kiyotaka Masaki , Naoko Isomura , Hiromi Yamamoto
Department of Mechanical Systems Engineering, Department of Bioresources Engineering
Okinawa Churashima Foundation
X-ray diffraction measurements (XRD) were obtained for the skeleton of an Acropora intermedia specimen and the shell of a Mizuhopecten yessoensis specimen in order to investigate the crystal structure of marine-derived calcium carbonate. The results implied the following conclusions. (1)The skeleton of Acropora intermedia is composed of aragonite, which is a metastable crystal. It is also oriented along a specific direction located at or near the tip. (2) The shell of Mizuhopecten yessoensis is composed of both calcite, which is stable crystal, and aragonite crystal. The region containing the scallop adductor is primarily composed of a structure formed of aragonite crystal. (3) The diffraction angles of certain aragonite crystal planes were shifted toward lower angles near the tip of the skeleton or the hinge of the shell. This result suggests the influence of strontium present in the specimens.
Key word: Calcium carbonate, X-Ray diffraction method, Aragonite, Calcite, Acropora intermedia,
Mizuhopecten yessoensis
12 Bulletin of Okinawa National College of Technology, No.9 (2015)