Identifikasi Karakteristik Batubara Melalui Analisis Proksimat dan Petrografi pada PT XYZ Provinsi Kalimantan Utara
Abstract
Abstract. Coal is a sedimentary rock derived from fossilized plants that have decomposed over millions of years so that they contain combustible elements. The elements in question are carbon (C), hydrogen (H), oxygen (O), and other additional elements such as sulfur (S), nitrogen (N), and other elements. The coal formation process is influenced by temperature, pressure, and geological time. So that coal has different characteristics, and these characteristics will affect the quality of coal The purpose of this research is to determine the characteristics of coal based on proximate and petrographic analyses. This research consists of several stages, namely petrographic analysis by making polished incision samples to determine the composition of maseral and mineral constituents of coal under a microscope and proximate analysis to determine the quality of coal. In addition, the determination of the deposition environment based on the maserals content of coal using the classification according to Diessel, 1992. Based on the results of the study, it is found that the characteristics of coal in the research area have an average moisture content (IM) of 26.3% (adb), an average ash content of 5.8% (adb), an average fly matter content (VM) of 38.72% (adb), tethered carbon (FC) of 28.53% (adb), and mineral matter reaching 15.2%.
Abstrak. Batubara yaitu batuan sedimen yang berasal dari fosil tumbuhan yang terdekompoisi selama berjuta-juta tahun sehingga mengandung unsur yang mudah terbakar. Unsur yang dimaksud berupa karbon (C), hidrogen (H), oksigen (O), dan unsur tambahan lainnya seperti belerang (S), Nitrogen (N) dan unsur lainnya. Proses pembentukan batubara dipengaruhi oleh suhu, tekanan, waktu geologi. Sehingga batubara memiliki karakteristik yang berbeda – beda dan karakteristik tersebut akan mempengaruhi kualitas dari batubara. Tujuan dari penelitian ini untuk mengetahui karakteristik batubara berdasarkan analisis proksimat dan petrografi. Penelitian ini terdiri dari beberapa tahapan yang dilakukan ini yaitu analisis petrografi dengan membuat sampel sayatan poles untuk mengetahui komposisi maseral dan mineral penyusun batubara dibawah mikroskop serta analisis proksimat untuk mengetahui kualitas batubara. Selain itu, dilakukan penentuan lingkungan pengendapan berdasarkan kandungan maseral batubara menggunakan klasifikasi menurut Diessel, 1992. Berdasarkan dari hasil penelitian didapatkan bahwa karakteristik batubara pada daerah penelitian memiliki kadar air (IM) rata – rata sebesar 26,3% (adb), kadar abu (Ash) rata – rata 5,8% (adb), kadar zat terbang (VM) rata – rata 38,72% (adb), karbon tertambat (FC) rata – rata 28,53% (adb) dan mineral matter mencapai 15,2%.
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