Loss-on-ignition in Hashilan Wetland sediment core, western Iran

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1. Verfasser: Safaierad, Reza
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2023
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_version_ 1867170416326344704
author Safaierad, Reza
author_facet Safaierad, Reza
collection Datos científicos de ciencias marinas y ambientales
contents The proxy data reported here are measured from a sediment core collected from the Hashilan Wetland in the Zagros Mountains of western Iran. For Loss-on-Ignition (LOI), samples with 1 cm3 volume were dried overnight at 105 °C and weighed. The dry samples were combusted at 550 °C for 4 hrs and at 950 °C for 2 hrs to determine OM and CaCO3 contents of the samples, respectively. The percentage of non-carbonate mineral matter (NCMM: LOI residue) was calculated using the following formula: 100 – LOI (in %). The analyses were carried out at the Faculty of Geography, University of Tehran.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_956209
institution PANGAEA
language en
publishDate 2023
publisher PANGAEA
record_format pangaea
spellingShingle Loss-on-ignition in Hashilan Wetland sediment core, western Iran
Safaierad, Reza
AGE; Atmospheric dust; Calculated; Combustion at 950°C; DEPTH, sediment/rock; Hashilan wetland; HashW_core; Holocene climate; HW; Ignition loss at 500°C; Ignition residue; loss on ignition; Loss on ignition; PEATC; Peat corer
The proxy data reported here are measured from a sediment core collected from the Hashilan Wetland in the Zagros Mountains of western Iran. For Loss-on-Ignition (LOI), samples with 1 cm3 volume were dried overnight at 105 °C and weighed. The dry samples were combusted at 550 °C for 4 hrs and at 950 °C for 2 hrs to determine OM and CaCO3 contents of the samples, respectively. The percentage of non-carbonate mineral matter (NCMM: LOI residue) was calculated using the following formula: 100 – LOI (in %). The analyses were carried out at the Faculty of Geography, University of Tehran.
title Loss-on-ignition in Hashilan Wetland sediment core, western Iran
topic AGE; Atmospheric dust; Calculated; Combustion at 950°C; DEPTH, sediment/rock; Hashilan wetland; HashW_core; Holocene climate; HW; Ignition loss at 500°C; Ignition residue; loss on ignition; Loss on ignition; PEATC; Peat corer
url https://doi.org/10.1594/PANGAEA.956209