Puzzled faces are often returned when people learn that my doctoral research involves analysing mud extracted from the bottom of a lake. Common questions include why? How? What does it look like? My interest in lake sediments was developed through my Undergraduate degree and addressing these queries is now an important part of my PhD at the University of Liverpool. In this post I will briefly outline some answers from a personal perspective.
Why? Lake sediment records have contributed hugely to our understanding of past environmental changes around the globe. Where a lake is fed by a river which drains the local catchment, sediment is transported through the fluvial system and deposited at the lake bottom. These sediments can be characterised using numerous parameters measured in the field or using advanced laboratory techniques and fluctuations in these measurements may indicate a change in local climate, land-use or vegetation cover. My research focuses on recovering sediment sequences from lakes in the English Lake District (Bassenthwaite and Brotherswater) which should contain records of extreme flood events which have occurred in the catchment in the past. If the sedimentological signature of discrete flood layers within a long sediment sequence can be deciphered, counting the number of such layers can provide insight into flood frequency and a relationship between grain size and river discharge may provide data on flood magnitude. Our sediment cores cover many centuries and, in some cases, millennia. These datasets will therefore be invaluable to river managers and policy makers who need a better context in which to place the current spate of extreme flood disasters witnessed in recent years and to develop more effective mitigation scenarios of future flood risk.
How? Many techniques have been developed to extract the soft sediments lying at a lake bottom. Preserving the internal structure of the sediment sequence is crucial, however the high water content of the mud means methods must be used which recover the lake sediments with minimal disturbance. For extracting sequences potentially many meters thick, we use a Russian-style sediment corer, which consists of a semi-cylindrical metal case with a rotating cover plate, with an optional manual hammer system that can be employed. At Liverpool, we have constructed a raft which enables coring to take place on a solid, well-anchored platform. The corer is lowered through the water column, with metal support rods attached as required to reach the desired depth. If the sediment proves difficult to penetrate, the hammer system is attached to the vertical supporting rods and a weight is lifted and dropped to drive the corer further into the basal sediments. When the desired depth is reached, the support rods are rotated clockwise, the cover carves through the sediment column and an undisturbed sediment sequence is captured within the casing.The corer is lifted to the surface, lain flat and the rotating motion is reversed, revealing a lovely stratigraphic sequence upon the cover. Each core drive (which can be 0.5, 1.0 or 1.5 m in length) is encased in PVC drainpipe and transported back to the laboratory.
What does it look like? In my short academic career, I have observed numerous textures, colours and smells associated with mud extracted from different lake environments. The spectrum of colour, for example, has ranged from white to black, incorporating greens, reds, greys and blues along the way. Examining the factors controlling these characteristics is far beyond the scope of a blog post, but I thoroughly recommend everyone volunteers to participate on the next lake coring trip run by their institution and grasp the opportunity to view mud in a whole new light.
Post written by Dan Schillereff