Seasonal release of Fe and Mn at the sediment-water interface in Aha Lake

The release of various harmful and poisonous elements from sediments to overlying water via pore water is one of the geochemical processes influencing and restricting the water quality of lakes. It is important for protecting and managing freshwater lakes to uncover and recognize the basic features and forming mechanism of this process. Iron     

高效液相色谱法测定喀斯特型高原深水水库中的微囊藻毒素的含量

建立了有效的检测微囊藻毒素LR和RR的方法,对固相萃取--高效液相色谱测定水中痕量藻毒素的部分实验过程进行了优化处理.流动相体积分数:0.080.b TFA的水+甲醇(色谱纯),体积流量:1.0ml/min,紫外检测波长:238nm,进样量:20uL;在该条件下,以HPLC测定MC-LR的检测限为5.0ng/L,MC-...     

Climatic changes documented by stable isotopes of sedimentary carbonate in Lake Sugan, northeastern Tibetan Plateau of China, since 2 kaBP

Lake Sugan at the northern edge of the Qaidam Basin was selected as the research object. The temporal sequence of sedimentary cores retrieved from Lake Sugan since 2 kaBP was reconstructed using the ^210Pb, AMS 14C and conventional 14C dating methods. Carbon and oxygen isotopes of carbonate in the fine-grained lake sediments were analysed. Combined with the changes of 8180 values of surface water and air temperature observation data in the study area, it might be thought that the δ^18O value of the carbonate indicates effective moisture, and the changes in δ^13C values are related to annual freeze-up duration of the lake and indirectly indicate air temperature changes in winter half year. From the above, the sequence of climatic changes in the region since 2 kaBP was established. The climatic changes experienced five stages： Warm-dry climate during 0-190 AD： cold-dry climate during 190-580 AD; warm-dry climate during 580-1200 AD （MWP）; cold-wet climate during 1200-1880 AD （LIA）; cold-dry climate during 1880-1950 AD： and climate warming since 1950s. The air temperature changes in winter half year reflected by carbon isotope since 2 kaBP are in good agreement with the historical literature records and other geologic records, which shows that the climate changes recorded by the stable isotopes from Lake Sugan since 2 kaBP are of universal significance.