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模拟研究变化水位和流速条件下鄱阳湖磷释放特征
作者: 童亚莉 梁涛 王凌青 李可欣  来源:Journal of Geographical Sciences 年份:2017 文献类型 :期刊
描述:Since the construction of the Three Gorges Dam,the Poyang Lake hydrological characteristics obviously changed.During the impoundment period of the Three Gorges Reservoir,the hydrodynamic factors of Poyang Lake varied.Water level dropped,the velocity decreased and water exchange time lengthened,which changed the release of phosphorous from sediments.In order to investigate how the hydrodynamic factors influence the release of phosphorous from sediments,we used a two-way annular flume device to simulate the release characteristics of phosphorous from sediments under variable water levels and velocities.We found that both water level rising and velocity increasing could enhance the disturbance intensity to sediments,which caused the increase of suspended solids(SS)concentration,total phosphorus(TP)concentration in the overlying water,and the ability that phosphorus released to overlying water from sediments enhanced as well:when overlying water velocity maintained 0.3 m/s,SS concentration increased to 4035.85 mg/L at the water level25 cm which was about 25 times compared to the minimum value and TP concentration in the overlying water also reached the maximum value at the water level 25 cm which was 1.2times that of the value at 10 cm;when water level maintained 15 cm,SS concentration increased to 4363.35 mg/L at the velocity of 0.5 m/s which was about 28 times compared to the value of 0 m/s,and TP concentration in the overlying water increased from 0.11 mg/L to 0.44mg/L.When the water level maintained 15 cm,the phosphorous release rate reached the maximum value of 4.86 mg/(md)at 0.4 m/s.The concentration of total dissolved phosphorous(TDP)and soluble reactive phosphate(SRP)both in overlying water and sediment-water interface were negatively correlated with p H.Using the parabolic equation,the optimum water level at a velocity of 0.3 m/s was calculated to be 0.57 cm,and the optimum velocity at water level of 15 cm was found to be 0.2 m/s.
全文:Since the construction of the Three Gorges Dam,the Poyang Lake hydrological characteristics obviously changed.During the impoundment period of the Three Gorges Reservoir,the hydrodynamic factors of Poyang Lake varied.Water level dropped,the velocity decreased and water exchange time lengthened,which changed the release of phosphorous from sediments.In order to investigate how the hydrodynamic factors influence the release of phosphorous from sediments,we used a two-way annular flume device to simulate the release characteristics of phosphorous from sediments under variable water levels and velocities.We found that both water level rising and velocity increasing could enhance the disturbance intensity to sediments,which caused the increase of suspended solids(SS)concentration,total phosphorus(TP)concentration in the overlying water,and the ability that phosphorus released to overlying water from sediments enhanced as well:when overlying water velocity maintained 0.3 m/s,SS concentration increased to 4035.85 mg/L at the water level25 cm which was about 25 times compared to the minimum value and TP concentration in the overlying water also reached the maximum value at the water level 25 cm which was 1.2times that of the value at 10 cm;when water level maintained 15 cm,SS concentration increased to 4363.35 mg/L at the velocity of 0.5 m/s which was about 28 times compared to the value of 0 m/s,and TP concentration in the overlying water increased from 0.11 mg/L to 0.44mg/L.When the water level maintained 15 cm,the phosphorous release rate reached the maximum value of 4.86 mg/(md)at 0.4 m/s.The concentration of total dissolved phosphorous(TDP)and soluble reactive phosphate(SRP)both in overlying water and sediment-water interface were negatively correlated with p H.Using the parabolic equation,the optimum water level at a velocity of 0.3 m/s was calculated to be 0.57 cm,and the optimum velocity at water level of 15 cm was found to be 0.2 m/s.
鄱阳湖沙化土地生态治理技术研究与示范
作者: 郑林 曹昀 丁明军 胡启武 李晓峰 贾玉连 詹选怀 李海涛 梁涛  来源:中国科技成果 年份:2015 文献类型 :期刊 关键词: 政府部门  示范  土地面积  滨湖地区  沙化治理  鄱阳湖地区  沙化土地  生态治理技术 
描述:鄱阳湖地区作为南方沙化的典型分布区,沙化土地面积3.89万公顷,主要分布于彭泽、湖口、都昌、星子、永修、新建等滨湖地区。当前,鄱阳湖沙化正以3~5米/年的速度扩展,甚至出现了“沙进人退”的状况,严重影响了当地居民的生产和生活,已引起科研机构和政府部门的高度重视。近几十年来,一些学者就鄱阳湖沙化土地的形成演化、景观结构、植被演替等方面进行了研究,但对鄱阳湖地区沙化土地演化过程、机理以及与北方荒漠化异同等问题目前尚没有形成明确、统一的结论,在沙化治理方面尽管也开展了一些相关工作,但还未探索出适宜于本地区成熟的沙化治理技术与模式。
全文:鄱阳湖地区作为南方沙化的典型分布区,沙化土地面积3.89万公顷,主要分布于彭泽、湖口、都昌、星子、永修、新建等滨湖地区。当前,鄱阳湖沙化正以3~5米/年的速度扩展,甚至出现了“沙进人退”的状况,严重影响了当地居民的生产和生活,已引起科研机构和政府部门的高度重视。近几十年来,一些学者就鄱阳湖沙化土地的形成演化、景观结构、植被演替等方面进行了研究,但对鄱阳湖地区沙化土地演化过程、机理以及与北方荒漠化异同等问题目前尚没有形成明确、统一的结论,在沙化治理方面尽管也开展了一些相关工作,但还未探索出适宜于本地区成熟的沙化治理技术与模式。
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