3 research outputs found
Seasonal dynamics of organic carbon and metals in thermokarst lakes from the discontinuous permafrost zone of western Siberia
Despite relatively good knowledge of the biogeochemistry of Siberian thermokarst lakes during summer base flow, their seasonal dynamics remains almost unexplored. This work describes the chemical composition of 130 thermokarst lakes ranging in size from a few m2 to several km2, located in the discontinuous permafrost zone. Lakes were sampled during spring flood, just after the ice break (early June), the end of summer (August), the beginning of ice formation (October) and during the full freezing season in winter (February). The lakes larger than 1000m2 did not exhibit any statistically significant control of the lake size on dissolved organic carbon (DOC), the major and trace element concentrations over three major open water seasons. On the annual scale, the majority of dissolved elements including organic carbon increased their concentration from 30 to 500 %, with a statistically significant (p summer>autumn>winter. The ice formation in October included several stages: first, surface layer freezing followed by crack (fissure) formation with unfrozen water from the deeper layers spreading over the ice surface. This water was subsequently frozen and formed layered ice rich in organic matter. As a result, the DOC and metal (Mn, Fe, Ni, Cu, Zn, As, Ba and Pb) concentrations were highest near the surface of the ice column (0 to 20 cm) and decreased by a factor of 2 towards the bottom. The main implications of discovered freeze-driven solute concentrations in thermokarst lake waters are enhanced colloidal coagulation and removal of dissolved organic matter and associated insoluble metals from the water column to the sediments. The measured distribution coefficients of a TE between amorphous organo-ferric coagulates and lake water (<0.45 ΞΌm) were similar to those reported earlier for Fe-rich colloids and low molecular weight (<1 kDa, or <1β2 nm) fractions of thermokarst lake waters, suggesting massive coprecipitation of TE with amorphous Fe oxyhydroxide stabilized by organic matter. Although the concentration of most elements was lowest in spring, this period of maximal water coverage of land created a significant reservoir of DOC and soluble metals in the water column that can be easily mobilized to the hydrological network. The highest DOC concentration observed in the smallest (<100m2) water bodies in spring suggests their strongly heterotrophic status and, therefore, a potentially elevated CO2 flux from the lake surface to the atmosphere
Seasonal dynamics of organic carbon and metals in thermokarst lakes from the discontinuous permafrost zone of western Siberia
Despite relatively good knowledge of the biogeochemistry of Siberian
thermokarst lakes during summer base flow, their seasonal dynamics remains
almost unexplored. This work describes the chemical composition of
~130 thermokarst lakes ranging in size from a few m2 to several
km2, located in the discontinuous permafrost zone. Lakes were sampled
during spring flood, just after the ice break (early June), the end of summer
(August), the beginning of ice formation (October) and during the full
freezing season in winter (February). The lakes larger than 1000 m2 did
not exhibit any statistically significant control of the lake size on
dissolved organic carbon (DOC), the major and trace element concentrations
over three major open water seasons. On the annual scale, the majority of
dissolved elements including organic carbon increased their concentration
from 30 to 500%, with a statistically significant (p < 0.05) trend
from spring to winter. The concentrations of most trace elements (TEs)
increased in the order spring > summer > autumn > winter. The ice
formation in October included several stages: first, surface layer freezing
followed by crack (fissure) formation with unfrozen water from the deeper
layers spreading over the ice surface. This water was subsequently frozen and
formed layered ice rich in organic matter. As a result, the DOC and metal
(Mn, Fe, Ni, Cu, Zn, As, Ba and Pb) concentrations were highest near the
surface of the ice column (0 to 20 cm) and decreased by a factor of 2
towards the bottom. The main implications of discovered freeze-driven solute
concentrations in thermokarst lake waters are enhanced colloidal coagulation
and removal of dissolved organic matter and associated insoluble metals from
the water column to the sediments. The measured distribution coefficients of
a TE between amorphous organo-ferric coagulates and lake water
(<0.45 ΞΌm) were similar to those reported earlier for Fe-rich
colloids and low molecular weight (<1 kDa, or <1β2 nm) fractions
of thermokarst lake waters, suggesting massive co-precipitation of TE with
amorphous Fe oxyhydroxide stabilized by organic matter. Although the
concentration of most elements was lowest in spring, this period of maximal
water coverage of land created a significant reservoir of DOC and soluble
metals in the water column that can be easily mobilized to the hydrological
network. The highest DOC concentration observed in the smallest
(2) water bodies in spring suggests their strongly
heterotrophic status and, therefore, a potentially elevated CO2 flux
from the lake surface to the atmosphere
Seasonal dynamics of organic carbon and metals in thermokarst lakes from the discontinuous permafrost zone of western Siberia
Despite relatively good knowledge of the biogeochemistry of Siberian thermokarst lakes during summer base flow, their seasonal dynamics remains almost unexplored. This work describes the chemical composition of 130 thermokarst lakes ranging in size from a few m2 to several km2, located in the discontinuous permafrost zone. Lakes were sampled during spring flood, just after the ice break (early June), the end of summer (August), the beginning of ice formation (October) and during the full freezing season in winter (February). The lakes larger than 1000m2 did not exhibit any statistically significant control of the lake size on dissolved organic carbon (DOC), the major and trace element concentrations over three major open water seasons. On the annual scale, the majority of dissolved elements including organic carbon increased their concentration from 30 to 500 %, with a statistically significant (p summer>autumn>winter. The ice formation in October included several stages: first, surface layer freezing followed by crack (fissure) formation with unfrozen water from the deeper layers spreading over the ice surface. This water was subsequently frozen and formed layered ice rich in organic matter. As a result, the DOC and metal (Mn, Fe, Ni, Cu, Zn, As, Ba and Pb) concentrations were highest near the surface of the ice column (0 to 20 cm) and decreased by a factor of 2 towards the bottom. The main implications of discovered freeze-driven solute concentrations in thermokarst lake waters are enhanced colloidal coagulation and removal of dissolved organic matter and associated insoluble metals from the water column to the sediments. The measured distribution coefficients of a TE between amorphous organo-ferric coagulates and lake water (<0.45 ΞΌm) were similar to those reported earlier for Fe-rich colloids and low molecular weight (<1 kDa, or <1β2 nm) fractions of thermokarst lake waters, suggesting massive coprecipitation of TE with amorphous Fe oxyhydroxide stabilized by organic matter. Although the concentration of most elements was lowest in spring, this period of maximal water coverage of land created a significant reservoir of DOC and soluble metals in the water column that can be easily mobilized to the hydrological network. The highest DOC concentration observed in the smallest (<100m2) water bodies in spring suggests their strongly heterotrophic status and, therefore, a potentially elevated CO2 flux from the lake surface to the atmosphere