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The Content Of Heavy Metal In Turmeric (Curcuma Domestica Val.) In The Volcanic Rocks Oligocene-Miocene Volcano, Biting Wonogiri, Central Java, Indonesia Yudiantoro, Dwi Fitri; Soesilo, Joko; Basuki Rahmad; Haty, Intan Paramita; Radityo Prakoso; Muhammad Nurcholis; Mirzam Abdurrachman; Wikaningrum, Temmy
Journal of Geoscience, Engineering, Environment, and Technology Vol. 9 No. 3 (2024): JGEET Vol 09 No 03 : September (2024)
Publisher : UIR PRESS

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25299/jgeet.2024.9.3.14896

Abstract

The Biting Wonogiri area is an area composed of Oligocene-Miocene volcanic deposits and volcanic deposits from Lawu Volcano. The rocks in this area consist of pyroclastic rocks, volcanic breccia, and dacite intrusions. Residents in this area more commonly grow herbal plants such as turmeric. Turmeric plants are mostly planted on old volcanic rocks, namely the Oligocene-Miocene age. By studying the planting patterns of residents, an analysis was carried out regarding the heavy metal chemical elements contained in turmeric. The research methodology was carried out using geological mapping to determine the distribution of the rocks that make up the research area and AAS analysis (Atomic Absorption Spectroscopy). This AAS method is used to determine heavy metal content. The heavy metal elements analyzed in turmeric were Hg, Pb, As, Fe, Al, and Mn. From the analysis results it was found that the heavy metal elements Hg, Pb, and As had very low levels, namely around 0.005-0.400 mg/Kg. Meanwhile, the elements Al, Fe, and Mg have high contents. Turmeric grown on dacite and volcanic breccia has higher Al (622.3-1362.76 mg/Kg) and Fe (271.32-806.27 mg/Kg) content compared to turmeric planted on sedimentary rock. Meanwhile, the metal element Mn varies around 6.85-122.01 mg/Kg. By knowing the content of these Western metal elements, it is hoped that turmeric, which contains heavy metal elements, can be used as a superior herbal herbal medicine. These metal elements, which are very important nutrients, come from old volcanic rocks.
Erupsi Semeru 1 Desember 2020: Kronologi Kejadian Aliran Piroklastik, Kondisi Pre-Eruptif, dan Laju Ekstrusi Material Volkanik Banggur, Wilfridus F S; Nareswari, Ratika Benita; Saina, Nazirah; Astyka Pamumpuni; Mirzam Abdurrachman; Estu Kriswati; Liswanto; Mukdas Sofian; Yadi Yuliandi; Kristianto; Sofyan Primulyana; Idham Andri Kurniawan
Jurnal Geologi dan Sumberdaya Mineral Vol. 25 No. 3 (2024): JURNAL GEOLOGI DAN SUMBERDAYA MINERAL
Publisher : Pusat Survei Geologi

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.33332/jgsm.geologi.v25i3.796

Abstract

Semeru merupakan gunungapi paling aktif di Jawa dengan tipe erupsi strombolian-vulkanian yang disertai pertumbuhan kubah lava. Erupsi eksplosif Semeru dapat menghasilkan guguran lava pijar dan runtuhan kubah lava yang disertai aliran piroklastik dengan jarak luncur mencapai 5-12 km ke arah selatan (Besuk Kembar dan Besuk Bang) atau tenggara (Besuk Kobokan) dari pusat erupsi. Pada 1 Desember 2020, terjadi aliran piroklastik dengan jarak luncur 11.5 km, yang merupakan jarak luncur terjauh sejak erupsi 2002. Rekonstruksi terhadap kronologi kejadian dan sebaran endapan aliran piroklastik 1 Desember 2020 secara detil dilakukan menggunakan data CCTV, press release, citra satelit, foto drone, portal berita, dan kanal media sosial. Kondisi pre-eruptif jangka pendek dikaji menggunakan citra satelit SAR Sentinel-1, Sentinel-2 dari MIROVA, dan frekuensi kegempaan. Algoritma MODVOLC digunakan untuk mengkaji laju ekstrusi produk material volkanik sebagai gambaran kondisi pre-eruptif jangka panjang. Rekonstruksi kejadian aliran piroklastik menunjukkan bahwa erupsi dimulai dengan guguran lava yang diikuti awan panas dengan beberapa perulangan dan kekuatan yang meningkat. Kondisi pre-eruptif sepanjang tahun 2020 menunjukkan perubahan morfologi bukaan kawah pusat, posisi titik runtuh guguran lava, serta posisi akumulasi material guguran di sekitar puncak yang menyebabkan arah luncuran aliran piroklastik lebih mengarah ke Besuk Kobokan. Sementara itu, peningkatan akumulasi volume dan laju ekstrusi material volkanik mengindikasikan kemungkinan peningkatan jarak luncuran ke depannya.