Tranter M.; Munhoven G.; Jones I.W.; Wadham J.L.; Huybrechts P.; Sharp M.J.; Brown G.H.; Hodson A.J.; Hodgkins R.(2002)
Chemical erosion in glacial environments is normally a consequence of chemical weathering reactions dominated by sulphide oxidation linked to carbonate dissolution and the carbonation of carbonates and silicates. Solute ...
Cooper R.J.; Wadham J.L.; Tranter M.; Hodgkins R.; Peters N.E.(2002)
Glacial bulk meltwaters and active-layer groundwaters were sampled from the proglacial zone of Finsterwalderbreen during a single melt season in 1999, in order to determine the geochemical processes that maintain high ...
Wadham J.L.; Tranter M.; Bottrell S.; Raiswell R.(2004)
Glacier beds may be host to a range of microbial communities, which drive oxic waters towards anoxia along certain hydrological flowpaths. Chemical and isotopic signatures in meltwaters from Finsterwalderbreen, a polythermal ...