

FOLLOWUS
1.Key Laboratory of Green and High-end Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China
2.Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China
3.University of the Chinese Academy of Sciences, Beijing 100049, China
hcwei@isl.ac.cn
收稿:2025-07-10,
网络首发:2026-04-09,
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Hongyu LI, Haicheng WEI, Aiying CHENG, 等. Hydrology and sediment supply in the largest lake system of Qaidam Basin, northeastern Qinghai-Xizang Plateau: insights from surface-sediment grain size[J/OL]. 海洋湖沼学报(英文), 2026,1-18.
LI Hongyu,WEI Haicheng,CHENG Aiying,et al.Hydrology and sediment supply in the largest lake system of Qaidam Basin, northeastern Qinghai-Xizang Plateau: insights from surface-sediment grain size[J].Journal of Oceanology and Limnology,
Hongyu LI, Haicheng WEI, Aiying CHENG, 等. Hydrology and sediment supply in the largest lake system of Qaidam Basin, northeastern Qinghai-Xizang Plateau: insights from surface-sediment grain size[J/OL]. 海洋湖沼学报(英文), 2026,1-18. DOI:
LI Hongyu,WEI Haicheng,CHENG Aiying,et al.Hydrology and sediment supply in the largest lake system of Qaidam Basin, northeastern Qinghai-Xizang Plateau: insights from surface-sediment grain size[J].Journal of Oceanology and Limnology, DOI:.
Climate warming and increased precipitation across the Qinghai-Xizang Plateau (QXP) have caused lake expansion
posing a threat to the safety of local infrastructure and ecosystems. Grain size in lake sediments is a reliable proxy for elucidating hydrological variations in these lakes. However
diverse sources of clastic fractions in lake sediments complicate the interpretation of hydrological changes based on grain-size records. We analyzed 94 surface-sediment samples from Hurleg and Toson lakes
the largest lake system of the Qaidam Basin
northeastern QXP
and explored the grain-size spatial distribution and its hydrological significance. Results demonstrate that fine silt (4–16 μm) is predominant in both lakes
followed by medium to coarse silt (16–63 μm)
and clay (<4 μm)
while sand (>63 μm) fraction was the least abundant. Using the end-member analysis (EMA)
we identified three end-members in Hurleg Lake (HEM1–HEM3) and four in Toson Lake (TEM1–TEM4). In Hurleg Lake
HEM1 and HEM2 mainly come from fluvial deposits from the Bayin River. HEM3 mainly comes from surface runoff and shoreline erosion. In Toson Lake
TEM1 represents typical lacustrine sediments
and TEM2 represents fine-grained terrestrial residual and gully input components. TEM3 originates mainly from aeolian transport and terrestrial residual. TEM4 is a dominant component of the subaqueous alluvial fan. Single-specimen unmixing suggested a differentiation between aeolian inputs and hydrodynamically sensitive components. Fine silt components (mode size 4.0–14.5 μm) are likely related to lake-level variations
whereas coarser silt components (mode size 18.7–51.8 μm) indicate regional dust activity. Notably
in Toson Lake
the fluvial sand components (mode size 66.9–111.5 μm) that were likely derived from western gully runoff
may represent a potential indicator of extreme hydrological events in the Qaidam Basin. These findings provide robust constraints on modern sedimentary processes for reconstructing the history of hydroclimatic changes using grain-size records in the northeastern QXP.
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