Mineralogical and Geochemical Clay Analysis for Portland Cement Quality Distribution: A Study Case From Ajibarang District, Central Java, Indonesia
DOI:
https://doi.org/10.25299/jgeet.2024.9.04.15812Keywords:
Claystone XRF, SEM, CementAbstract
Nowadays, the development of infrastructure has caused an increase in the need for cement. To determine the suitability of the raw materials used in cement production, an assessment must be carried out on the quality anMineralogical and Geochemical Clay Analysis for Portland Cement Quality Distribution: A Study Case From Ajibarang District, Central Java, Indonesiad suitability of the cement raw materials. This research was conducted in Halang Formation of the Tipar Kidul area and around Banyumas Regency, Central Java. The methods used are X-ray fluorescence (XRF) and scanning electron microscopy (SEM). Data from XRF analysis generally shows SiO2 values from 26.83% to 57.75%, Al2O3 values from 11.18% to 20.23%, and Fe2O3 values from 3.21% to 8.76%. Judging from the aluminum index (AI) content, the ideal cement raw materials are two samples with a proportion of 3.17% to 3.22%. The results of SEM analysis show that there are illite, calcite, quartz and smectite minerals in the claystone research area. Based on data, almost 75% of the claystone survey area was found to be suitable as a raw material for cement. This research has a positive impact on the characterization of limestone as a raw material for cement by utilizing geochemical analysis and electron microscopy to achieve a more comprehensive understanding of the evaluation of limestone quality.
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References
Adhari, M. R., & Hidayat, R. (2023). A geological overview of the limestone members of the Woyla Group of Sumatra, Indonesia. Journal of Geoscience, Engineering, Environment, and Technology, 8(3), 189–195.
Amin, M. H. A., & Susilo, B. K. (2019). Lingkungan pengendapan Formasi Tapak daerah Samudra, Kabupaten Banyumas, Jawa Tengah. Proceeding of Innovation of Engineering and Science Research, 252–259.
Astuti, B. S., Isnaniawardhani, V., Abdurrokhim, & Sudradjat, A. (2017). Micro Tectonic At North Serayu Basin, Central Java: Case Study At Type Locality of Rambatan Formation. 233–237.
Astuti, B. S., Isnaniawardhani, V., Abdurrokhim, & Sudradjat, A. (2019). Sedimentation Process of Rambatan Formation in Larangan Brebes, North Serayu Range, Central Java. Indonesian Journal on Geoscience, 6(2), 141–151.
Bouma, A. H. (1964). Developments In Sedimentology Turbidites.
Brahmantyo, B., & Bandono. (2006). Klasifikasi Bentuk Muka Bumi (Landform) untuk Pemetaan Geomorfologi pada Skala 1:25.000 dan Aplikasinya untuk Penataan Ruang. Jurnal Geoaplika, 1(2), 071–078.
Djuri, M. (1996). Peta Geologi Regional Lembar Purwokerto-Tegal, skala 1:100.000.
Gibran, A. K., & Kusworo, A. (2020). Fasies dan Lingkungan Pengendapan Formasi Kanikeh , Cekungan Bula, Maluku. RISET Geologi Dan Pertambangan, 30(2), 171–186.
Gibran, A. K., Kusworo, A., Wahyudiono, J., Sunan, H. L., Aeni, D. N., & Alghazali, A. (2020). Reservoir Characteristic of Triassic Sandstone, Eastern Seram, Maluku, Indonesia. IOP Conference Series: Materials Science and Engineering, 982(1).
Gibran, A. K., Setijadi, R., Purwasatriya, E. B., Ananda, D. R., & Nabil, M. I. (2022). Biostratigrafi Dan Sedimentologi Plio-Pleistosen Daerah Bumiayu - Tonjong, Jawa Tengah. Jurnal Geologi Kelautan, 20(1), 33–44.
Gibran, A., Kusworo, A., Wahyudiono, J., & Purwasatriya, E. (2022). Proses Diagenesis Batupasir Formasi Kanikeh, Seram Bagian Timur, Maluku, IndonesiaSandstone Diagenesis Process of Kanikeh Formation, Eastern Seram, Molucca, Indonesia. Journal of Geology and Mineral Resources, 23(200), 113–122.
Gifford, J. N., Platt, B. F., Yarbrough, L. D., O’reilly, A. M., & Al Harthy, M. (2020). Integrating petrography, x-ray fluorescence, and u-pb detrital zircon geochronology to interpret provenance of the mississippian hartselle sandstone, USA. Journal of Geology, 128(4), 337–370.
Goldstein, J. I., Newbury, D. E., Michael, J. R., Ritchie, N. W. M., Henry, J., Scott, J., & Joy, D. C. (2018). Scanning Electron Microscopy and X-Ray Microanalysis.
Grabau, A. W. (1904). On The Classification Of Sedimentary Rocks. American geologist.
Isnaniawardhani, V. (2017). Prinsip dan Aplikasi Biostratigrafi.
Itamiya, H. (2019). Analysis of the surface microtextures and morphologies of beach quartz grains in Japan and implications for provenance research. Progress in Earth and Planetary Science, 6(1).
Kurniasih, A., Adha, I., Dalimunthe, H. L., Setyawan, R., Khorniawan, W. B., Qadaryati, N., Jayanti, A. G. R., & Wijaya, F. P. (2023). Biostratigraphic Interpretation of Lutut Beds, Kerek Formation, Based on Foraminifera Fossils. Journal of Geoscience, Engineering, Environment, and Technology, 8(2), 105–111.
Marin, J., Winarno, T., & Fairuz, S. N. (2022). Characteristics of Kedondong Trass and Bobos Trass as Cement Raw Material, Cirebon, West Java, Indonesia. Journal of Geoscience, Engineering, Environment, and Technology, 7(1), 27–33.
Pettijohn, F. J. (1975). Sedimentary Rock Third Edition. Harper & Row.
PT. Sinar Tambang Arthalestari. (2023). Database Hasil Survey.
Purwasatriya, E. B., Gibran, A. K., Aditama, M. R., & Waluyu, G. (2021). Sedimentologi dan Tektonostratigrafi Formasi Halang di Cekungan Banyumas serta Potensinya untuk Reservoir Hidrokarbon. Jurnal Geologi Dan Sumberdaya Mineral, 22(3), 153–163.
Rizkianto, Y., Choiriah, S. U., Subandrio, A., Haty, I. P., Isnani, D. K., Nurwantari, N. A., Syah Darmawa, M. A., & Wirandoko, H. (2023). Trace Fossils Of The Selorejo Formation, Rembang Zone, North East Java Basin, Indonesia. Journal of Geoscience, Engineering, Environment, and Technology, 8(3), 183–188.
Rohmana, R. C., & Achmad, A. (2019). Analisis Sedimentologi dan Stratigrafi untuk Rekonstruksi Model Lingkungan Pengendapan : Mengungkap Proses Pembentukan Formasi Tapak , Abstrak Objek studi difokuskan pada Formasi Tapak yang terendapkan pada Miosen Akhir – Pliosen Akhir di Sub-Cekungan Ban. Geoscience Dan Teknologi, 2 no.3(58), 126–134.
Safira, F., Purwasatriya, E. B., & Gibran, A. K. (2023). Early to Middle Miocene Dissectec Arc of Karangsambung Area: A Case Study of Waturanda and Penosogan Formations Provenance. Journal of Earth and Marine Technology (JEMT), 3(2), 124–140.
Sun, M. (2014). What’s The Difference Between Subaerial And Subaqueous Originated Subaqueous Pyroclastic Rocks. Chinese Academy of Sciences.
Theng, B. K. (2019). Clay Mineral Catalysis of Organic Reactions.
Walker, R. G. (1992). Facies Models And Modern Stratigaphic Concepts.
Welton, J. E. (2020). SEM Petrology Atlas. In SEM Petrology Atlas (Issue 4).
Wijaya. (2005). Kelayakan Kimia Mineral Lempung sebagai Bahan Baku Semen Portland di Desa Tritih Lor, Kecamatan Jeruklegi, Kabupaten Cilacap : Studi Kasus Pengembangan Eksplorasi Mineral Lempung sebagai Bahan Baku Semen di PT. Semen Cibinong Tbk (Persero) Pabrik Cilacap. Gadjah Mada Yogyakarta.
Wilkins, A. D. (2014). Terminology and the classification of fine grained sedimentary rocks – is there a difference between a claystone, a mudstone and a shale? Geology, 1950, 1–12.
Worden, R. H., & Morad, S. (2003). Clay mineral cements in sandstones. Blackwell Pub.
Zerlinda, D. R., & Aditama, M. R. (2021). Interpretasi Geologi Daerah Cidora Dan Sekitarnya, Kecamatan Lumbir, Kabupaten Banyumas, Jawa Tengah. Jurnal Pendidikan Dan Teknologi Indonesia, 1(2).
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