Hematite is a canted antiferromagnet with reddish color that occurs widely on Earth and
Mars. Identification and quantification of hematite is conveniently achieved through its …

Abstract The Paleocene-Eocene Thermal Maximum (PETM) hyperthermal,~ 56 million years
ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. During the …

The quest for a sustainable environment and combating global warming, carbon capture,
and storage (CCS) has become the primary resort. A complete shift from non-renewable …

It is common in the fields of rock and environmental magnetism to unmix magnetic mineral
components using statistical methods that decompose various types of magnetization curves …

Ferrihydrite is among the most common precursors for iron-oxide formation in soils and
sediments. Previous studies proposed a three-stage process for ferrihydrite transformation to …

Over the past decade, incessant research efforts have been devoted to the development of
iron oxide nanoparticles (IONPs) for wastewater industry. Past research has witnessed the …

Soil magnetic susceptibility (κ) has potential to be used as a pedoenvironmental indicator
from which mineralogy, pedogeochemical, pedogeomorphological and pedogenic …

Abstract The La Colonia Formation is an Upper Cretaceous to Paleogene shallow marine
sedimentary unit in Chubut Province (Patagonia), Argentina that preserves important …

In recent years, increasing interest in loess studies has focused on qualitative and
quantitative paleoclimatic reconstruction using the imperfect antiferromagnetic mineral …

The increase in food consumption and limitations in food production areas requires
improved fertilizer efficiency. Slow-or controlled-release fertilizers are an alternative for …