Page 30 - 2021年第52卷第10期

（2）：202-207 .
［ 27］ 王帅帅，罗齐彬，杨亚新，等 . 趋势面法提取相山地区地气异常及应用效果评价［J］. 科学技术与工程，
2020，20（13）：5058-5065 .

Temporal and spatial variation of water quantity exchange between surface water and
groundwater in typical district of Sanjiang Plain

1，2 1，2 3 4 1，2 1，2
SHU Longcang ，YIN Xiaoran ，YUAN Yajie ，LU Yan ，LU Chengpeng ，LIU Bo
（1. College of Hydrology and Water Resources， Hohai University，Nanjing 210098，China；
2. State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering，Hohai University，Nanjing 210098，China；
3. Heilongjiang Monitoring Center of Hydrology and Water Resources，Harbin 150001，China；
4. Jiamusi Monitoring Center of Hydrology and Water Resources，Jiamusi 154002，China）

Abstract：The exchange of water quantity between surface water and groundwater is a complex process that
is influenced by topographic factors， hydrologic factors and hydrogeologic factors. This article focused on
the analysis of a representative district of the Sanjiang Plain with four rivers as the research area bound⁃
ary： Songhuajiang， Heilongjiang， Naolihe and Wusulijiang rivers. The spatial-temporal variation of water
quantity exchange between river and groundwater in representative river sections of this region was investigat⁃
ed based on field hydrogeological investigations and analysis of the spatial distribution of river and ground⁃
water level dynamics from 2000 to 2018. The findings revealed that there is a strong hydraulic connection
between surface water and groundwater at representative river sections in the Sanjiang plain，which is signif⁃
icantly or highly correlated in more than 50% of the years during the study period. The Fujin section of
Songhuajiang River had the strongest correlation whilst Caijuzi section of Naolihe River and Haiqing section
of Wusulijiang River had a correlation between Fujin section of Songhuajiang River and Qindeli section of
Heilongjiang River. The weakest correlation was observed at the Qindeli section of Heilongjiang River. On a
perennial scale， the Caijuzi section of Naolihe River is ground water recharged by surface water， whereas
the Fujin section， the Haiqing section and the Qindeli section， of Songhuajiang River， Wusulijiang River
and Heilongjiang River respectively are all surface water recharged by groundwater. The perennial average
water quantity exchange per unit width of the river and groundwater in Fujin section of Songhuajiang River
-2 3 -5 3
is 10 （m /d·m），Qindeli section of Heilongjiang River is 10 （m /d·m），Caijuzi section of Naolihe River
-3
-3
3
3
is 10 （m /d·m）， and Haiqing section of Wusulijiang River is 10 （m /d·m） The correlation coefficient
.
and the magnitude of water quantity exchange per unit width of the river and groundwater had a positive re⁃
lationship， the bigger the correlation coefficient value， the higher the water quantity exchange per unit
width， and the results of MK trend test show that the water quantity exchange between surface water and
groundwater in representative river sections has a decreasing trend，the trend is significant in Haiqing sec⁃
tion of Wusulijiang River， Fujin section of Songhuajiang River has the least decreasing trend. The water
quantity exchange of surface water and groundwater in the Fujin section of Songhuajiang River is strongly
dominated by annual and interannual fluctuation and only June showed a significant decreasing trend on in⁃
terannual scale，which does not constitute the significant annual decreasing trend，therefore the water quan⁃
tity exchange relation changes frequently wish a weak regularity. The Qindeli section of Heilongjiang River
is dominated by annual and interannual fluctuation，comparable to the Songhuajiang River，though to a less⁃
er extent，there is no significant interannual decreasing trend thus it does not constitute the significant an⁃
nual decreasing trend. The interannual fluctuation dominate the Caijuzi section of Naolihe River and there
was a significant decreasing trend from January to May，but it does not increase the fluctuation in interan⁃
nual scale and not constitute the significant annual decreasing trend. The Haiqing section of Wusulijiang
River is mainly dominated by annual fluctuation， the significant decreasing trend from June to September
and December increase the fluctuation in interannual scale and constitute the significant annual decreasing
trend. The findings of this study can serve as a scientific basis for the evaluation of water resources in the
typical district of Sanjiang Plain，as well as a theoretical reference for the scientific development and utili⁃
zation of water resources in this region.
Keywords：rivers；aquifer；surface water and groundwater；water quantity exchange；spatial-temporal variation
（责任编辑：耿庆斋）

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