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Low Flow Trends and Frequency Analysis in the Blue Nile Basin, Ethiopia
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作者 Kidist Assefa Mamaru A. Moges 《Journal of Water Resource and Protection》 2018年第2期182-203,共22页
Low flow analysis provides crucial information for the planning and design water resource development, risk assessment and environmental flow management. Understanding the low flow regimes and evaluating the magnitude... Low flow analysis provides crucial information for the planning and design water resource development, risk assessment and environmental flow management. Understanding the low flow regimes and evaluating the magnitudes for incorporating in water resources management is vital for the countries like Ethiopia where demand for water is increasing. However, there were hardly enough studies in understanding the trends of low flow and frequency analysis. Therefore, this study focuses on evaluation of the trends in low flows and regional low flow analysis in the Blue Nile Basin, Ethiopia. In order to carry out the study, 15 river sub-basins in the Blue Nile Basin were selected based on the long term data availability and presence of quality of data. The 3-day sustained low flow (3d-slf), the 7-day sustained low flow (7d-slf) and the 14-day sustained low flow (14d-slf) models were used to extract the data from the daily time series stream data obtained from MoWIE. Trends in low flow were analyzed separately by using Mann-Kendall (MK) trend test. Low flow frequency analysis was used to estimate the long term low flow quantiles. In addition, regional analysis for estimating the quantiles for ungaged catchments was also developed based on the regional growth curve and catchment characteristic of drainage basins. The results indicated that 3d-slf, 7d-slf and 14d-slf models of low flow series indicated no significant difference for each station at 95% CI. Out of the 15 selected stations, 12 of stations have indicated decreasing;two stations indicated increasing and remaining one station with no trend. Mainly decreasing trend was associated with the land cover and climate change which results in increasing runoff and evapotranspiration respectively. Weibull distribution—GEV and LGN was found best fit based on the L-Moment Ratio Diagram (L-MRD). Hence quantile estimations have indicated diminishing magnitudes of low flow quintiles for 2 - 500 years return periods. Regional low frequency analysis has provided a very good relati 展开更多
关键词 MANN-KENDALL Low Flow L-MRD PWM REGIONALIZATION blue nile basin
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蓝尼罗河盆地喀土穆凹陷构造演化及烃源岩发育特征 被引量:1
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作者 孔令武 张树林 +1 位作者 段晓梦 方勇 《中国海上油气》 CAS CSCD 北大核心 2017年第5期22-29,共8页
对蓝尼罗河盆地喀土穆凹陷构造演化特征进行了分析,重新厘定了构造演化阶段,并对主力烃源岩发育特征及油气来源进行了深入分析。研究表明:喀土穆凹陷的形成与演化受控于中非剪切带的活动,该凹陷经历了裂陷Ⅰ期、裂陷Ⅱ期及拗陷期等构造... 对蓝尼罗河盆地喀土穆凹陷构造演化特征进行了分析,重新厘定了构造演化阶段,并对主力烃源岩发育特征及油气来源进行了深入分析。研究表明:喀土穆凹陷的形成与演化受控于中非剪切带的活动,该凹陷经历了裂陷Ⅰ期、裂陷Ⅱ期及拗陷期等构造演化阶段。早白垩世裂陷Ⅰ期的强裂陷作用是湖相烃源岩发育的主要时期,综合烃源岩地化指标及油-源对比分析认为Abu Jinn组烃源岩为喀土穆凹陷的主力烃源岩。喀土穆凹陷Abu Jinn组烃源岩与穆格莱德盆地Abu Gabra组主力烃源岩沉积环境类似,为弱氧化-弱还原的沉积环境,且水体较淡。不同构造位置处Abu Jinn组烃源岩有机质类型和甾烷分布差别较大。Abu Jinn组烃源岩热演化程度主要受埋藏深度的控制,但火山活动促进了Abu Jinn组烃源岩的热演化,烃源岩成熟度受火成岩影响范围约为火成岩上下200 m范围。 展开更多
关键词 蓝尼罗河盆地 喀土穆凹陷 构造演化 烃源岩 沉积环境 有机质类型 热演化
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