A thorough understanding of cave seepage waters is necessary to interpret geochemical variations in speleothem calcite in terms of changing surface climatic conditions at a particular site. Here we present the hydrochemistry of ten cave drip waters from a karst system in SE Australia based on up to 5.5 years of monitoring. Discharge was continuously measured at six sites and manually at the other sites. Dripwater samples were analysed for pH, electrical conductivity, cations and anions at all sites at monthly or more frequent intervals. Each drip possesses a unique chemistry, and not all drip waters responded to antecedent short-term hydrological variations. For example, the hydrochemical behaviour of three adjacent drips at a bedrock depth...
Palaeoclimate research using speleothems has significantly increased over the last decade, owing to ...
Five stalagmite drip-waters in the Grotte de Villars, Dordogne, have been monitored from early 1997...
Cave drip water response to surface meteorological conditions is complex due to the heterogeneity of...
A thorough understanding of cave seepage waters is necessary to interpret geochemical variations in ...
A better knowledge of dripwater hydrology in karst systems is needed to understand the palaeoclimate...
Speleothem trace element chemistry is an important component of multi-proxy records of environmental...
Speleothems (cave deposits), used for palaeoenvironmental reconstructions, are deposited from cave d...
Speleothems (cave deposits), used for palaeoenvironmental reconstructions, are deposited from cave ...
Cave monitoring provides a crucial link between hydrological and climate processes and how they may ...
The study of how cave drip-water discharge responds to recharge events is fundamental to evaluating ...
Trace element variations in ancient cave speleothems are often interpreted as indicators of changes ...
The identification of vadose zone hydrological pathways that most accurately transmit climate signal...
Paleoclimate studies are an important tool to aid our current knowledge and understanding of past cl...
Groundwater geochemistry is used to investigate flow paths, water residence times, and rock-water in...
A 4-year study in a central Texas cave quantifies multiple mechanisms that control dripwater composi...
Palaeoclimate research using speleothems has significantly increased over the last decade, owing to ...
Five stalagmite drip-waters in the Grotte de Villars, Dordogne, have been monitored from early 1997...
Cave drip water response to surface meteorological conditions is complex due to the heterogeneity of...
A thorough understanding of cave seepage waters is necessary to interpret geochemical variations in ...
A better knowledge of dripwater hydrology in karst systems is needed to understand the palaeoclimate...
Speleothem trace element chemistry is an important component of multi-proxy records of environmental...
Speleothems (cave deposits), used for palaeoenvironmental reconstructions, are deposited from cave d...
Speleothems (cave deposits), used for palaeoenvironmental reconstructions, are deposited from cave ...
Cave monitoring provides a crucial link between hydrological and climate processes and how they may ...
The study of how cave drip-water discharge responds to recharge events is fundamental to evaluating ...
Trace element variations in ancient cave speleothems are often interpreted as indicators of changes ...
The identification of vadose zone hydrological pathways that most accurately transmit climate signal...
Paleoclimate studies are an important tool to aid our current knowledge and understanding of past cl...
Groundwater geochemistry is used to investigate flow paths, water residence times, and rock-water in...
A 4-year study in a central Texas cave quantifies multiple mechanisms that control dripwater composi...
Palaeoclimate research using speleothems has significantly increased over the last decade, owing to ...
Five stalagmite drip-waters in the Grotte de Villars, Dordogne, have been monitored from early 1997...
Cave drip water response to surface meteorological conditions is complex due to the heterogeneity of...