Magnetic hysteresis measurement

Knowledge graph centered on Magnetic hysteresis measurement with 68 nodes and 143 connections. Top connected: climatological variability, sediment transport, Manganese oxidation, ferric hydroxide precipitation, Graben formation.

Method synopsis

Rock fragments measured for magnetic hysteresis properties and isothermal remanent magnetization to identify magnetic mineral carriers and domain states.

Synthesized from method descriptions across 2 papers using this protocol.

Procedure from a recent peer-reviewed implementation

Steps below were extracted from the most recent peer-reviewed implementation of this protocol in the corpus — Post-Depositional Fluid Flow in Jurassic Sandstones of the Uncompahgre Uplift: Insights From Magnetic Fabrics (2020), Frontiers in Earth Science. Implementations in other papers (listed below) may differ.

1. Magnetic hysteresis measurements
   Magnetic hysteresis experiments and Isothermal Remanent Magnetization (IRM) experiments were performed at room temperature on rock fragments to identify the nature of AMS carriers. Field strength up to 1.5 T was applied to saturate specimens magnetically
   Quantities: Two representative specimens with contrasting colorsDuration: Not specifiedConditions: Room temperature
   Equipment: MicroMag 3900-04 vibrating sample magnetometer

Typical Equipment

• MicroMag 3900-04 vibrating sample magnetometer

Output Measurements

• coercivity
• saturation magnetization
• magnetic mineralogy

Papers Using This Protocol (2)

Species Studied With This Protocol

Places Where Used