H2020Индивидуална стипендия2017–2019

DryMIN · Mineral weathering in the unsaturated zone from the molecular to macro scale

„Хоризонт 2020“ — Действия „Мария Склодовска-Кюри“

Период: 2017-01-23 → 2019-01-22
Финансиране от ЕС: 183 455 €
Участници: 1
Схема: MSCA-IF

Линиите свързват координатора с партньорите.

Накратко на български

Разграждането на минерали в почвата се изучава при различна влажност, например как се променят химичните реакции при изсушаване и намокряне. Това помага за по-доброто предвиждане на цикъла на въглерода и хранителните вещества при промяна на валежите.

Този кратък обзор е генериран от изкуствен интелект

Кратко обяснение, генерирано от езиков модел по текста на CORDIS. Оригиналът е по-долу.

Резултати накратко

Mineral weathering in the unsaturated zone from the molecular to macro scale

"""Mineral weathering in the unsaturated zone from the molecular to macro scale (DryMIN)” Earth’s shallow subsurface, or “critical zone,” is of fundamental importance for supporting terrestrial life and maintaining water quality. A vital part of the critical zone is the unsaturated region located nearest to the surface. This zone is also most likely to be affected by future global change due to altered rainfall patterns and evapotranspiration rates across the globe. In order to predict how long-term variations in the water budget will impact nutrient and carbon cycling it is necessary to evaluate the influence of water saturation on mineral weathering reactions. The objective of the research was to elucidate the fundamental mechanisms governing reaction rates as a function of water availability from the molecular to macro scale. This was achieved through a combination of experimental studies, geochemical modelling, and analytical techniques. Experimental results indicated that mineral weathering reactions are sensitive to the availability of water below a threshold of water availability. Mineral dissolution-precipitation reactions were observed to proceed in the presence of an adsorbed water film only, but the extent of reaction was limited below 100% humidity. At 100% humidity, reactions proceeded at a rate similar to water-unlimited conditions. Column experiments also revealed that element release during weathering is sensitive to wetting and drying cycles. This implies that weathering rates are likely to be impacted by changes in water availability and evaporation-recharge patterns. Our experimental results will help to develop a mechanistic reactive transport model that can better predict reaction rates as a function of water saturation. This research has significant implications for the maintenance of a sustainable nutrient supply for natural and agricultural vegetation, the carbon cycle, and remediation of groundwater resources, issues critical to the long-term sustainable growth of our society."

Текст от CORDIS, на английски · Данни: CORDIS, © Европейски съюз

Цел на проекта

"Mineral weathering in the unsaturated zone from the molecular to macro scale (DryMIN)”Earth’s shallow subsurface, or “critical zone,” is of fundamental importance for supporting terrestrial life and maintaining water quality. Perhaps the most vital part of the critical zone is the unsaturated region located nearest to the surface. It is in the unsaturated zone where most plants acquire their nutrients, and where most organic carbon degrades. This zone is also most likely to be affected by future global change due to altered rainfall patterns and evapotranspiration rates across the globe. In order to predict how long-term variations in the water budget will impact nutrient and carbon cycling it is necessary to evaluate the influence of water saturation on mineral weathering reactions. The objective of the proposed research is to elucidate the fundamental mechanisms governing reaction rates as a function of water availability from the molecular to macro scale. This will be achieved through a combination of three scale-spanning experimental studies: 1) humidity buffer experiments investigating molecular-scale changes to mineral surfaces, 2) pore-scale microfluidic experiments, and 3) macro-scale flow-through column experiments. Experimental results will lead to the development of a mechanistic reactive transport model that can better predict reaction rates as a function of water saturation. This research has significant implications for the maintenance of a sustainable nutrient supply for natural and agricultural vegetation, the carbon cycle, and remediation of groundwater resources, issues critical to the long-term sustainable growth of our society. Through this research programme I will: 1) have opportunities for mobility between multiple institutions in Europe, 2) gain tangible skills in analytical techniques, 3) improve transferable communication and management skills, and 4) establish a lasting multi-disciplinary, collaborative European research network.""

Оригинален текст от CORDIS (на английски).

Участници

UNIVERSITY COLLEGE LONDON · LondonКоординаторОбединеното кралство