Search Results (3)

Micronutrient deficiencies in human diets, often exacerbated by soil degradation, pose a significant global health challenge. Glacial flour, fine sediments produced by glacial erosion, may offer a sustainable, low-cost solution to improve soil fertility and enhance micronutrient availability in crops. This study evaluates the potential of glacial flour soil amendments from glaciers with two contrasting lithologies—basaltic Sólheimajökull (Iceland) and metasedimentary Chhota Shigri (Himalaya)—to enrich soybeans (Glycine max var. Black Jet) with essential nutrients while assessing the risk associated with potentially toxic elements. In a controlled glasshouse experiment, soybeans were grown in artificial soils amended with five doses of glacial flour (0.5–20 T ha⁻¹) and analysed for 18 elements. Results demonstrated enhanced uptake of key nutrients such as Zn, Fe, Mo, and Se, particularly in Icelandic glacial flour treatments, supporting the potential for crop biofortification. However, Himalayan flour led to arsenic (As) accumulation at higher doses, exceeding food safety limits. Multivariate clustering revealed two distinct element uptake behaviours: oxyanion-mediated and mimicking elements (Mo, Se, Sr, As) and those driven by plant demand (macronutrients, Fe, Mn, Zn). These findings highlight glacial flour’s potential for nutrient enrichment but also of potentially toxic elements, underscoring the need for source-specific screening to ensure safe agricultural application in deglaciating regions. Full article

Icelandic topsoil sediments, as confirmed by numerous scientific studies, represent the largest and the most important European source of mineral dust. Strong winds, connected with the intensive cyclonic circulation in the North Atlantic, induce intense emissions of mineral dust from local sources all year and carry away these fine aerosol particles for thousands of kilometers. Various impacts of airborne mineral dust particles on local air quality, human health, transportation, climate and marine ecosystems motivated us to design a fully dynamic coupled atmosphere–dust numerical modelling system in order to simulate, predict and quantify the Icelandic mineral dust process including: local measurements and source specification over Iceland. In this study, we used the Dust Regional Atmospheric Model (DREAM) with improved Icelandic high resolution dust source specification and implemented spatially variable particle size distribution, variable snow cover and soil wetness. Three case studies of intense short- and long-range transport were selected to evaluate the model performance. Results demonstrated the model’s capability to forecast major transport features, such as timing, and horizontal and vertical distribution of the processes. This modelling system can be used as an operational forecasting system, but also as a reliable tool for assessing climate and environmental Icelandic dust impacts. Full article

In this work, we present the results of element content in river sediments and soil of the Rangárvellir river in southern Iceland as well as in the volcano ash from the Eyjafjallajökull eruption in 2010. Severe natural catastrophes have devastating impact on the environment. We selected the Rangárvellir area located in the vicinity of Mt Hekla, Iceland’s most active volcano, for our study. This study site is ideal to investigate wind and water erosion and sediment transport processes of two main glaciers rivers: the Eystri-Rangá and the Ytri-Rangá and the Hroarslækur River. Sediments of these rivers consist of volcano materials, ash and lava. In order to assess the sediment dynamics, we collected sediment, soil and volcanic ash. The fractioning of the elements was carried out using sequential extractions. The distribution of Si indicates that the sediments originate from the same geochemical basis. Li and partly B exist in the first phase of volcanic ash and river sediments but not in the mobile phases of soils. In the mobile phase of volcanic ash, P was found but it did not exist in the first phase of soil and sediments. These results suggest the different chemical fingerprints in the water sediments and surrounding soil. Full article