YAO Haikun, SHI Kebin, KONG Xuanzhao, et al. Analysis of the Characteristics and Trend of Runoff and Sediment of Reservoir in the Upper Reaches of the Weigan River in the Past 60 Years[J]. 2023, 37(5): 121-129.
DOI:
YAO Haikun, SHI Kebin, KONG Xuanzhao, et al. Analysis of the Characteristics and Trend of Runoff and Sediment of Reservoir in the Upper Reaches of the Weigan River in the Past 60 Years[J]. 2023, 37(5): 121-129. DOI: 10.13870/j.cnki.stbcxb.2023.05.015.
Analysis of the Characteristics and Trend of Runoff and Sediment of Reservoir in the Upper Reaches of the Weigan River in the Past 60 Years
Studying the runoff and sediment characteristics and trends of sandy rivers in arid and semi-arid regions is of great significance for water and sediment regulation and prediction in the basin. Based on the macro (micro) perspective
the characteristics and trends of sandy rivers in arid and semi-arid areas were studied in detail
in order to provide theoretical help for flow and sediment regulation and prediction in river basins. In this study
the umulative distance method
ITA method and ITA-CB method were used to calculate the inflow flow and sediment transport rate of Kezier Reservoir
meanwhile the characteristics and trends of flow and sediment transport rate were systematically analyzed from the three scales of intrayear
interannual and interdecade scales. The results showed that:(1) The distribution characteristics of flow and sediment were highly similar in the year
with the highest value in July and the lowest value in March and January
respectively
with strong volatility and obvious differences on the interannual scale. (2) The annual inbound flow in the past 58 years showed an upward trend with an increasing tendency
and in summer it showed an upward trend with a weakening tendency
among which the upward trend of the high-value area weakened
and it was necessary to pay attention to the extreme climate of drought. (3) The annual sediment transport rate showed an upward trend
and the trend characteristics under the quarterly scale showed a downward trend
among which the downward trend in summer and autumn tended to weaken
and it showed a tendency to strengthen in winter. Compared with traditional analysis methods
ITA and ITA-CB methods could effectively identify the microscopic trends within the sequence
and were more helpful for analyzing the changes of regional flow and sediment in detail.
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