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Silica Sand Identification using ALOS PALSAR Full Polarimetry on The Northern Coastline of Rupat Island, Indonesia

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@article{IJASEIT920,
   author = {Husnul Kausarian and Josaphat Tetuko Sri Sumantyo and Hiroaki Kuze and Detri Karya and Good Fried Panggabean},
   title = {Silica Sand Identification using ALOS PALSAR Full Polarimetry on The Northern Coastline of Rupat Island, Indonesia},
   journal = {International Journal on Advanced Science, Engineering and Information Technology},
   volume = {6},
   number = {5},
   year = {2016},
   pages = {568--573},
   keywords = {Silica Sand; ALOS PALSAR Full Polarimetry; Rupat Island; XRF},
   abstract = {Silica sand is one of the minerals which relatively abundant in Indonesia. One of the areas with abundant of silica sand distribution is the northern coastline of Rupat Island, Bengkalis district, Riau province, Indonesia. The distribution of silica sand in this island identified only on the northern coastline in this island. Some selected sample of silica sand was measured to get the percentage of silica sand mineral’s content using X-Ray Fluorescence (XRF). Two adjacent scenes of ALOS PALSAR full-polarimetry were used. The physical properties of silica sand sample such as dielectric constant were measured using dielectric probe kit in the frequency range from 0.3 to 3.0 GHz and used for calculating the backscattering coefficient and the difference characteristics of silica sand with another object. Freeman-Durdeen and Yamaguchi techniques were used to get the scattering decomposition of physical scattering from the incoherent object model based. Surface scattering is the clearest of Scattering decomposition to show silica sand identification compares with other decompositions. From surface scattering, the backscattering coefficient value of silica sand was calculated starting from -59 dB until -52 dB. These values were given by the surface roughness condition, where the roughness is slightly rough planar. The flat condition supported by the grain size of silica sand particles that have almost the same size and shape, that were conducted by using microscopic photograph testing.},
   issn = {2088-5334},
   publisher = {INSIGHT - Indonesian Society for Knowledge and Human Development},
   url = {http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=920},
   doi = {10.18517/ijaseit.6.5.920}
}

EndNote

%A Kausarian, Husnul
%A Sri Sumantyo, Josaphat Tetuko
%A Kuze, Hiroaki
%A Karya, Detri
%A Panggabean, Good Fried
%D 2016
%T Silica Sand Identification using ALOS PALSAR Full Polarimetry on The Northern Coastline of Rupat Island, Indonesia
%B 2016
%9 Silica Sand; ALOS PALSAR Full Polarimetry; Rupat Island; XRF
%! Silica Sand Identification using ALOS PALSAR Full Polarimetry on The Northern Coastline of Rupat Island, Indonesia
%K Silica Sand; ALOS PALSAR Full Polarimetry; Rupat Island; XRF
%X Silica sand is one of the minerals which relatively abundant in Indonesia. One of the areas with abundant of silica sand distribution is the northern coastline of Rupat Island, Bengkalis district, Riau province, Indonesia. The distribution of silica sand in this island identified only on the northern coastline in this island. Some selected sample of silica sand was measured to get the percentage of silica sand mineral’s content using X-Ray Fluorescence (XRF). Two adjacent scenes of ALOS PALSAR full-polarimetry were used. The physical properties of silica sand sample such as dielectric constant were measured using dielectric probe kit in the frequency range from 0.3 to 3.0 GHz and used for calculating the backscattering coefficient and the difference characteristics of silica sand with another object. Freeman-Durdeen and Yamaguchi techniques were used to get the scattering decomposition of physical scattering from the incoherent object model based. Surface scattering is the clearest of Scattering decomposition to show silica sand identification compares with other decompositions. From surface scattering, the backscattering coefficient value of silica sand was calculated starting from -59 dB until -52 dB. These values were given by the surface roughness condition, where the roughness is slightly rough planar. The flat condition supported by the grain size of silica sand particles that have almost the same size and shape, that were conducted by using microscopic photograph testing.
%U http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=920
%R doi:10.18517/ijaseit.6.5.920
%J International Journal on Advanced Science, Engineering and Information Technology
%V 6
%N 5
%@ 2088-5334

IEEE

Husnul Kausarian,Josaphat Tetuko Sri Sumantyo,Hiroaki Kuze,Detri Karya and Good Fried Panggabean,"Silica Sand Identification using ALOS PALSAR Full Polarimetry on The Northern Coastline of Rupat Island, Indonesia," International Journal on Advanced Science, Engineering and Information Technology, vol. 6, no. 5, pp. 568-573, 2016. [Online]. Available: http://dx.doi.org/10.18517/ijaseit.6.5.920.

RefMan/ProCite (RIS)

TY  - JOUR
AU  - Kausarian, Husnul
AU  - Sri Sumantyo, Josaphat Tetuko
AU  - Kuze, Hiroaki
AU  - Karya, Detri
AU  - Panggabean, Good Fried
PY  - 2016
TI  - Silica Sand Identification using ALOS PALSAR Full Polarimetry on The Northern Coastline of Rupat Island, Indonesia
JF  - International Journal on Advanced Science, Engineering and Information Technology; Vol. 6 (2016) No. 5
Y2  - 2016
SP  - 568
EP  - 573
SN  - 2088-5334
PB  - INSIGHT - Indonesian Society for Knowledge and Human Development
KW  - Silica Sand; ALOS PALSAR Full Polarimetry; Rupat Island; XRF
N2  - Silica sand is one of the minerals which relatively abundant in Indonesia. One of the areas with abundant of silica sand distribution is the northern coastline of Rupat Island, Bengkalis district, Riau province, Indonesia. The distribution of silica sand in this island identified only on the northern coastline in this island. Some selected sample of silica sand was measured to get the percentage of silica sand mineral’s content using X-Ray Fluorescence (XRF). Two adjacent scenes of ALOS PALSAR full-polarimetry were used. The physical properties of silica sand sample such as dielectric constant were measured using dielectric probe kit in the frequency range from 0.3 to 3.0 GHz and used for calculating the backscattering coefficient and the difference characteristics of silica sand with another object. Freeman-Durdeen and Yamaguchi techniques were used to get the scattering decomposition of physical scattering from the incoherent object model based. Surface scattering is the clearest of Scattering decomposition to show silica sand identification compares with other decompositions. From surface scattering, the backscattering coefficient value of silica sand was calculated starting from -59 dB until -52 dB. These values were given by the surface roughness condition, where the roughness is slightly rough planar. The flat condition supported by the grain size of silica sand particles that have almost the same size and shape, that were conducted by using microscopic photograph testing.
UR  - http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=920
DO  - 10.18517/ijaseit.6.5.920

RefWorks

RT Journal Article
ID 920
A1 Kausarian, Husnul
A1 Sri Sumantyo, Josaphat Tetuko
A1 Kuze, Hiroaki
A1 Karya, Detri
A1 Panggabean, Good Fried
T1 Silica Sand Identification using ALOS PALSAR Full Polarimetry on The Northern Coastline of Rupat Island, Indonesia
JF International Journal on Advanced Science, Engineering and Information Technology
VO 6
IS 5
YR 2016
SP 568
OP 573
SN 2088-5334
PB INSIGHT - Indonesian Society for Knowledge and Human Development
K1 Silica Sand; ALOS PALSAR Full Polarimetry; Rupat Island; XRF
AB Silica sand is one of the minerals which relatively abundant in Indonesia. One of the areas with abundant of silica sand distribution is the northern coastline of Rupat Island, Bengkalis district, Riau province, Indonesia. The distribution of silica sand in this island identified only on the northern coastline in this island. Some selected sample of silica sand was measured to get the percentage of silica sand mineral’s content using X-Ray Fluorescence (XRF). Two adjacent scenes of ALOS PALSAR full-polarimetry were used. The physical properties of silica sand sample such as dielectric constant were measured using dielectric probe kit in the frequency range from 0.3 to 3.0 GHz and used for calculating the backscattering coefficient and the difference characteristics of silica sand with another object. Freeman-Durdeen and Yamaguchi techniques were used to get the scattering decomposition of physical scattering from the incoherent object model based. Surface scattering is the clearest of Scattering decomposition to show silica sand identification compares with other decompositions. From surface scattering, the backscattering coefficient value of silica sand was calculated starting from -59 dB until -52 dB. These values were given by the surface roughness condition, where the roughness is slightly rough planar. The flat condition supported by the grain size of silica sand particles that have almost the same size and shape, that were conducted by using microscopic photograph testing.
LK http://ijaseit.insightsociety.org/index.php?option=com_content&view=article&id=9&Itemid=1&article_id=920
DO  - 10.18517/ijaseit.6.5.920