First archaeointensity results from the historical period of Cambodia, Southeast Asia

Understanding variations of the geomagnetic field has applications regarding the behavior of the Earth's outer core, dating of archeological artifacts, and the phenomenon that shields life from solar radiation. However, archaeointensity studies of the Holocene have been mostly limited to localities in Europe and the Middle East; archaeomagnetic surveys from Southeast Asia are almost non-existent. This investigation aims to establish a secular variation curve of geomagnetic field intensity for Cambodia. We sampled ancient iron smelting mounds from the Khmer Empire, located in present day Cambodia, and are analyzing them for paleointensity. The specimens are thought to be from the historical period, likely between 1000-1500 CE. Our samples, which include furnace fragments, iron slag, and ceramic tuyères, contain magnetic minerals that record the paleointensity of Earth's magnetic field at the time it was fired. Using the IZZI paleointensity method (Yu et al., 2004), which gradually replaces the sample's natural remanent magnetization with a thermal remanent magnetization obtained in a known lab field, we can determine the geomagnetic intensities preserved in these specimens. Based on our preliminary experiments, the tuyères, and perhaps also the fresh slag, will in all likelihood yield the most ideal results. Following additional measurements from these best-fit samples, we will determine the paleointensities of Cambodia for the time period from which the artifacts originated. This will commence the establishment of regional geomagnetic reference curves in Southeast Asia and also improve the global model.