Michael Schaefer

Algae as nutritional and functional food sources: revisiting our understanding

Fate of arsenic before and after chemical-enhanced washing of an arsenic-containing soil in Hong Kong

Arsenic-containing soil from geogenic source in Hong Kong: Leaching characteristics and stabilization/solidification

Effect of dissolved oxygen concentration on iron efficiency: Removal of three chloroacetic acids

Soil amendments for immobilization of potentially toxic elements in contaminated soils: A critical review

Mobility and phytoavailability of As and Pb in a contaminated soil using pine sawdust biochar under systematic change of redox conditions

The limitations of applying zero-valent iron technology in contaminants sequestration and the corresponding countermeasures: The development in zero-valent iron technology in the last two decades (1994–2014)

Central nervous system sarcoidosisdiagnosis and management

Remediation of heavy metal(loid)s contaminated soils – To mobilize or to immobilize?

Nanoscale zero valent iron and bimetallic particles for contaminated site remediation

Fe(II) Sorption on a Synthetic Montmorillonite. A Combined Macroscopic and Spectroscopic Study

Arsenic and Environmental Health: State of the Science and Future Research Opportunities

Redox Transformation of Arsenic by Fe(II)-Activated Goethite (α-FeOOH)

Sea Level Rise Induced Arsenic Release from Historically Contaminated Coastal Soils

Sarcoidosis and Its Neurological Manifestations

Transport of Non-Newtonian Suspensions of Highly Concentrated Micro- And Nanoscale Iron Particles in Porous Media: A Modeling Approach

A review on the adsorption of heavy metals by clay minerals, with special focus on the past decade

Peat formation concentrates arsenic within sediment deposits of the Mekong Delta

Sarcoidosis of the pineal gland

Arsenic Concentrations in Paddy Soil and Rice and Health Implications for Major Rice-Growing Regions of Cambodia

Interpreting nanoscale size-effects in aggregated Fe-oxide suspensions: Reaction of Fe(II) with Goethite

Spectroscopic Evidence for Interfacial Fe(II)−Fe(III) Electron Transfer in a Clay Mineral

Arsenic release metabolically limited to permanently water-saturated soil in Mekong Delta