147 results for group: agrogeology-2
Silicate weathering in the Ganges alluvial plain
Patrick J. Frings, Wim Clymans, Guillaume Fontorbe, William Gray, Govind J. Chakrapani, Daniel J. Conley, Christina De La Rocha
Abstract
The Ganges is one of the world’s largest rivers and lies at the heart of a body of literature that investigates the interaction between mountain orogeny, weathering and global climate change. Three regions can be recognised in the Ganges basin, with the Himalayan orogeny to the north and the plateaus of peninsular India to the south together delimiting the Ganges alluvial plain. Despite constituting approximately 80%
of the basin, weathering processes in the peninsula and alluvial plain have received little ...
oxalate secretion by ectomycorrhizal Paxillus involutus is mineral-speciic and controls calcium weathering from minerals
A. schmalenberger, A. L. Duran, A. W. Bray, J. Bridge, s. Bonneville, L. G. Benning, M. e. Romero-Gonzalez, J. R. Leake, s. A. Banwart
Abstract
oxalate secretion by ectomycorrhizal Paxillus involutus is mineral-speciic and controls calcium weathering from minerals
Geochemical carbon dioxide removal potential of Spain
Liam A. Bullock, Juan Alcalde, Fernando Tornos, Jose-Luis Fernandez-Turiel
Abstract
Many countries have made pledges to reduce CO2 emissions over the upcoming decades to meet the Paris Agreement targets of limiting warming to no >1.5 °C, aiming for net zero by mid-century. To achieve national reduction targets, there is a further need for CO2 removal (CDR) approaches on a scale of millions of tonnes, necessitating a better understanding of feasible methods. One approach that is gaining attention is geochemical CDR, encompassing (1) in-situ injection of CO2-rich gases into Ca and Mg-rich rocks for geological storage by mineral carbonation, (2) ...
Effects of precipitation seasonality, irrigation, vegetation cycle and soil type on enhanced weathering – modeling of cropland case studies across four sites
Giuseppe Cipolla, Salvatore Calabrese, Amilcare Porporato, Leonardo V. Noto1
Abstract
Enhanced weathering (EW) is a promising strategy for carbon sequestration, but several open questions remain regarding the actual rates of dissolution in conditions
of natural hydroclimatic variability in comparison to laboratory experiments. In this context, models play a pivotal role, as they allow exploring and predicting EW dynamics under different environmental conditions. Here a comprehensive hydro biogeochemical model has been applied to four cropland case studies (i.e., Sicily and the Padan plain in Italy and California and Iowa in the USA) character...
The Theoretical Potential of Hondsrug Glacial Rock Dust as Soil Remediator in The Netherlands
Niels Christian Olfert
Abstract
Agriculture in the Netherlands is a major source of ammonia (NH3) emissions. Deposited nitrogen levels in the Netherlands reached 2-3 times their critical value at the start of 2020. Excess nitrogen in soil may cause declines in biodiversity and ecosystemic disequilibrium. This may lead to acidic and decalcified soils that are less capable of retaining nutrients. The mineral fines in rock dust are proven agents in soil remediation and remineralization. Glacial moraine deposits are a branded source of rock dust and are contained in the glacial till of the “Hondsrug” area, a boulder clay ridge in the northeast...
Potential accumulation of toxic trace elements in soils during enhanced rock weathering
Xavier Dupla, Benjamin Möller, Philippe C. Baveye, Stéphanie Grand
Abstract
Terrestrial enhanced rock weathering (ERW) is a carbon dioxide removal technology that aims at accelerating one of the most powerful negative feedbacks on Earth's climate, the chemical weathering of silicates. To achieve this, ERW proposes to spread ground silicate rock on agricultural soils. According to many models, global application rates of 40 tonnes of ground basaltic rock per hectare and per year would be necessary to sequester a significant amount of CO2, representing up to 24% of the current net annual increase in atmospheric CO2. When assessing the viabil...
Assessment of the enhanced weathering potential of different silicate minerals to improve soil quality and sequester CO2
Emily Pas, Mathilde Hagens, Rob Comans
Abstract
Enhanced weathering is a negative emission technology that involves the spread of crushed silicate minerals and rocks on land and water. When applied to agricultural soils, the resulting increase in soil pH and release of nutrients may co-benefit plant productivity. Silicate minerals and rocks differ in their enhanced weathering potential, i.e., their potential for both carbon dioxide (CO2) sequestration and soil quality improvements. However, studies comparing silicate minerals and rocks for this dual potential are lacking. Therefore, we compared the enhanced weathering potential of olivine ...
Impacts of dissolved phosphorus and soil-mineral-fluid interactions on CO2 removal through enhanced weathering of wollastonite in soils
Cameron Wood, Anna L.Harrison, Ian M.Power
The weathering of silicate minerals removes carbon dioxide (CO2) from the atmosphere over geologic timescales and is also investigated as an engineered strategy to mitigate climate change on decadal timescales. “Enhanced rock weathering” (ERW) is a carbon dioxide removal strategy that involves spreading of pulverized, highly reactive silicate rock at the Earth's surface such as within agricultural and natural soils. The rate and efficacy of ERW in agricultural soils to remove CO2 is difficult to quantify owing to the complex geochemical environment including biological-mineral-fluid-atmosphere intera...
