Key research themes
1. How do different chemical fractionation methods characterize phosphorus forms in biosolids and soils, and what implications does this have for phosphorus availability and environmental impact?
This research theme focuses on the application and evaluation of chemical fractionation techniques to identify and quantify phosphorus (P) fractions in stabilized biosolids, agricultural soils, and sediments. The goal is to understand the forms of P present, such as labile, moderately labile, and stable organic and inorganic phosphorus, and how these forms relate to bioavailability, fertilizer efficiency, and environmental risks like eutrophication. Insights into fractionation methods such as modified Hedley fractionation, sequential chemical extractions, and analytical spectroscopy provide a mechanistic basis for optimizing P use and mitigating losses.
2. What are the mechanisms and challenges of phosphorus recovery from wastewater and sludge, and how do iron and other chemical interactions influence recovery efficiency?
This area investigates the chemical and process engineering aspects of phosphorus recovery from wastewater and sewage sludge —a critical strategy to replenish phosphorus resources while preventing eutrophication. Studies focus on the impact of iron on P binding and recovery, the efficacy of struvite precipitation for P recovery, and the valorization of multi-nutrient waste streams. Understanding the iron-phosphorus chemistry that governs P availability in treatment systems is essential for developing cost-effective and environmentally sound recovery technologies.
3. How do sedimentary phosphorus fractions reflect historical nutrient loading and influence internal phosphorus cycling and eutrophication in aquatic ecosystems?
Research in this theme examines phosphorus fractionation in lake and river sediments to reveal legacy accumulation, internal loading potential, and biogeochemical cycling linked to eutrophication dynamics. Sequential extraction approaches differentiate bioavailable, detrital, organic, and refractory P pools within sediments, enabling spatial and temporal assessment of anthropogenic impacts. Understanding sediment P chemistry helps predict sedimentary contributions to harmful algal blooms and guides nutrient management strategies in freshwater systems.