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东平湖生态水位研究

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基于东平湖1960-2020年日水位序列,利用Mann-Kendall法、滑动T法和小波分析法对东平湖水位突变点进行确定,分析年均水位变化趋势和日水位变化特点,探讨水位变化对东平湖湿地空间演变的影响,结合年内展布法和变异性范围法(RVA法)对东平湖生态水位进行研究.结果表明:东平湖水位突变年为1989年;水位上升使东平湖入湖口和出湖口湿地空间发生了明显的演变;水位突变前年内展布法1和2计算的逐月生态水位分别在38.11~39.46 m和36.94~38.24 m之间,突变前生态水位月保障程度较高,水位突变后长期保持高水位;东平湖生态水位应以水位突变后水位序列进行计算,年内展布法1和2计算的逐月生态水位在39.83~40.55 m和37.59~38.27 m之间,高低水位历时各年份差别较大;年内展布法1计算的东平湖生态水位可以保证湿地不退化,结合湿地水下高程和芦苇生长期确定了东平湖适宜水位;东平湖汛期可设置汛限动态水位,不仅可以使大汶河洪水资源化,而且可以保障东平湖生态系统的健康.
Studies on ecological water level of Dongping Lake
The Mann-Kendall method,moving t-test technique,and wavelet analysis were used to de-termine the water level mutation point of Dongping Lake,analyze the trend of the annual average water level change,and characterize the daily water level change based on the daily water level sequence of Dongping Lake from 1960 to 2020.The impact of water level change on the spatial evolution of Dong-ping Lake wetland was discussed.The ecological water level of Dongping Lake was studied using the annual spreading method and the variability range method(RVA)in combination.The results showed that(1)the abrupt change of water level occurred in 1989,and the rise of the water level has caused a significant evolution in the wetland space at the entrance and exit of Dongping Lake;(2)the monthly ecological water levels calculated with the annual spreading methods 1 and 2 before the water level mu-tation varied between 38.11 and 39.46 m and between 36.94 and 38.24 m,respectively,the monthly protection degree of the ecological water level before the mutation was relatively high,and the water level remained high for a long time after the water level mutation;(3)the ecological water level of Dongping Lake was calculated based on the water level sequence after the abrupt change,the monthly ecological water level calculated by the annual spreading methods 1 and 2 within the year ranged from 39.83 to 40.55 m and from 37.59 to 38.27 m,and the duration of high and low water levels varies greatly in different years;(4)the ecological water level of Dongping Lake calculated with annual spreading method 1 during the year ensured that the wetland will not degrade,at the same time,by combining the underwater elevation of the wetland with the growth period of the reeds,the suitable wa-ter level of Dongping Lake can be determined;(5)by setting the dynamic water level of the Dongping Lake flood limit,the Dawen River flood can be resourced and the health of Dongping Lake ecosystem can be guaranteed.

Dongping Lakewater level mutationwetlandsannual spreading methodecological wa-ter levelsuitable water level

刘新阳、刘贺、苏强、冀健红、于晓龙、徐洪增、陈豪、路民

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华北水利水电大学,河南郑州 450046

河南水利与环境职业学院,河南 郑州 450008

山东黄河河务局工程建设中心,山东济南 250011

东平湖管理局东平管理局,山东东平 271500

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东平湖 水位突变 湿地 年内展布法 生态水位 适宜水位

2024

海洋湖沼通报
山东海洋湖沼学会

海洋湖沼通报

CSTPCD北大核心
影响因子:0.464
ISSN:1003-6482
年,卷(期):2024.46(6)