水文
水文
수문
Journal of China Hydrology
2015年
5期
82-90
,共9页
李雨%王雪%周波%袁德忠%陈金凤
李雨%王雪%週波%袁德忠%陳金鳳
리우%왕설%주파%원덕충%진금봉
南水北调中线工程%汉江中下游%水量特性%水质特性%变化趋势
南水北調中線工程%漢江中下遊%水量特性%水質特性%變化趨勢
남수북조중선공정%한강중하유%수량특성%수질특성%변화추세
south-to-north water diversion project%the middle and lower reaches of the Hanjiang River%water quantity characteristics%water quality characteristics%change trend
为研究南水北调中线工程调水前,汉江中下游的水量和水质本底特性及变化趋势,选择汉江中下游6个水文站及4个水质观测断面,采用数理统计、Mann-Kendall检验和Spearman秩次检验法,分别从水量和水质两个方面进行了分析。研究结果表明:(1)对比分析历史长序列流量资料,1999~2013年间汉江中下游地区处于偏枯期;(2)汉江中下游水量的年际变化较大,极值比介于2.7~3.3之间。水量年内各月分配变化也较大,汛期径流量占全年的63%~66%,非汛期仅占全年的34%~37%;(3)汉江中下游地区各水文测站的年均流量序列,总体上随时间变化的趋势均不显著,但经历了1980~1990的偏丰期及1990~2013的偏枯期;(4)汉江中下游地区的水质达标情况较好,大部分年份的水质均优于III类水质标准,且水质无显著的变化趋势。
為研究南水北調中線工程調水前,漢江中下遊的水量和水質本底特性及變化趨勢,選擇漢江中下遊6箇水文站及4箇水質觀測斷麵,採用數理統計、Mann-Kendall檢驗和Spearman秩次檢驗法,分彆從水量和水質兩箇方麵進行瞭分析。研究結果錶明:(1)對比分析歷史長序列流量資料,1999~2013年間漢江中下遊地區處于偏枯期;(2)漢江中下遊水量的年際變化較大,極值比介于2.7~3.3之間。水量年內各月分配變化也較大,汛期徑流量佔全年的63%~66%,非汛期僅佔全年的34%~37%;(3)漢江中下遊地區各水文測站的年均流量序列,總體上隨時間變化的趨勢均不顯著,但經歷瞭1980~1990的偏豐期及1990~2013的偏枯期;(4)漢江中下遊地區的水質達標情況較好,大部分年份的水質均優于III類水質標準,且水質無顯著的變化趨勢。
위연구남수북조중선공정조수전,한강중하유적수량화수질본저특성급변화추세,선택한강중하유6개수문참급4개수질관측단면,채용수리통계、Mann-Kendall검험화Spearman질차검험법,분별종수량화수질량개방면진행료분석。연구결과표명:(1)대비분석역사장서렬류량자료,1999~2013년간한강중하유지구처우편고기;(2)한강중하유수량적년제변화교대,겁치비개우2.7~3.3지간。수량년내각월분배변화야교대,신기경류량점전년적63%~66%,비신기부점전년적34%~37%;(3)한강중하유지구각수문측참적년균류량서렬,총체상수시간변화적추세균불현저,단경력료1980~1990적편봉기급1990~2013적편고기;(4)한강중하유지구적수질체표정황교호,대부분년빈적수질균우우III류수질표준,차수질무현저적변화추세。
In order to evaluate the characteristics and change trend of the water quantity and quality in the middle and lower reaches of the Hanjiang River before the running of the middle route of the south-to-north water diversion project (MR-SNWDP), 6 hydrometry stations and 4 water quality monitoring sections were selected, and mathematical statistics, Mann-Kendall test and Spearman test were used for the analysis. The results are follows: (1) 1999~2013 are in the dry season in the middle and lower reaches of the Hanjiang River based on a comparative analysis of the long term observed flow data; (2) The flow in this area indicate a considerable inter-annual variation with a proportion (maximum/minimum) between 2.7 and 3.3. The variation of annual flow in this area is also noticeable. Runoff during the flood season is accounting for 63 percent to 66 percent of the total runoff of the year, and runoff during the dry season is accounting for 34%~37% of the total runoff in the whole year. (3) The change trend of the flow-time series in this area is not noticeable. However, it experienced two periods: the wet seasons (from 1980 to 1990) and the dry seasons (from 1990 to 2013). (4) The water quality in this area is good according to the analysis of the water quality monitoring data, which can attain the standards of grade III in the most years, and the change trend of water quality in this area is also not noticeable.