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What is soil structure?

Soil structure is the result of the spatial arrangement of the solid soil particles and their associated pore space. Aggregation mainly depends on the soil composition and texture, but is also strongly influenced by other factors such as biological activity, climate, geomorphic processes or the action of fire. Structure is a typical morphological soil property, which …[Read More]

Geosciences Column: Dating a bivalve

Just as the rings on a tree can be used to determine its age, the bands on a bivalve’s shell can tell us the how long it’s been around for. Warm, food-filled waters lead to greater growth in the summer and low plankton abundance (the principle food source for filter-feeding molluscs) leads to limited growth …[Read More]

Sweeping soot out of the atmosphere

Efforts to slow the rate of global temperature rise in the 21st Century have for some time focussed on non-CO2 species or so-called ‘short-lived forcers’. As far as aerosols are concerned, black carbon (often referred to as soot) has been the main avenue to explore due to its capacity to warm the atmosphere by absorbing …[Read More]

EGU 2014 – got an idea?

Have a great idea for a conference session but haven’t quite put it into practice? Now’s your chance! Until this time next month (13 September) you can submit your session ideas and take part in organising the scientific programme for the EGU General Assembly in 2014. What you need to do: Take a look at …[Read More]

Guest Blog: A Summer of Volcanic Observation in Ecuador (3)

David Litchfield completed a second undergraduate degree in Geosciences with the Open University and is currently studying part-time for an MSc in Geophysical Hazards at UCL. He has a broad interest in hazard monitoring methods and how geoscientists communicate their findings with those who need it, and retains a strong connection with the Andean highlands …[Read More]