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Titlebook: Earth Surface Processes and Environmental Changes in East Asia; Records From Lake-ca Kenji Kashiwaya,Ji Shen,Ju Yong Kim Book 2015 Springer

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31#
發(fā)表于 2025-3-26 22:22:54 | 只看該作者
Possible Age Models for Lake Onuma Lacustrine Sediments Based on Tuffs Recovered in Three Cores,ion. Volcanic deposits Ko-a (1929?AD), Ko-c. (1856?AD), Ko-d (1640?AD), and possibly Ko-c. (1694?AD) were successfully identified with the help of radiocarbon age dating, .Cs radioactivity measurement, and chemical analyses, to construct an age model of these cores.
32#
發(fā)表于 2025-3-27 04:44:18 | 只看該作者
33#
發(fā)表于 2025-3-27 06:23:14 | 只看該作者
34#
發(fā)表于 2025-3-27 10:28:54 | 只看該作者
Conclusion: The end of “Butter Side Up”e sources and that their mixture ratio was almost constant since the 1920s. On the other hand, the δ.N of two cores show a similar trend with increasing δ.N from the 1950s–1960s to the present time. It is attributed to the increase in the δ.N value of planktonic material reflecting anthropogenic nitrogen inflow to the lake.
35#
發(fā)表于 2025-3-27 16:06:37 | 只看該作者
https://doi.org/10.1007/978-0-8176-8286-6 and precipitation near the Lake Onuma system is different in summer and winter. This indicates that the earth-surface processes in snowfall areas are different for the summer period (rainfall) and winter period (snow accumulation/snowmelt).
36#
發(fā)表于 2025-3-27 18:24:28 | 只看該作者
Recent Eutrophication and Environmental Changes in the Catchment Inferred from Geochemical Propertie sources and that their mixture ratio was almost constant since the 1920s. On the other hand, the δ.N of two cores show a similar trend with increasing δ.N from the 1950s–1960s to the present time. It is attributed to the increase in the δ.N value of planktonic material reflecting anthropogenic nitrogen inflow to the lake.
37#
發(fā)表于 2025-3-27 23:43:14 | 只看該作者
38#
發(fā)表于 2025-3-28 03:36:04 | 只看該作者
39#
發(fā)表于 2025-3-28 09:29:24 | 只看該作者
40#
發(fā)表于 2025-3-28 10:45:41 | 只看該作者
https://doi.org/10.1007/978-3-322-83399-0ter samples and inlet and outlet samples were collected. The concentrations of major dissolved species in the samples revealed that the lake water is Ca.-HCO.. type, but that the Ca. and HCO.. levels are relatively low. The water has high dissolved SiO. concentrations, which suggests favorable condi
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