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地下水中氮化物转换的氧化还原条件 总被引:3,自引:0,他引:3
地下水中氧化还原电位影响着各种氮化物的分布和浓度变化。计算资料已经用于确定这些化合物之间的Eh—pH边界值。计算条件与地下水中不同形式氮化物的实际资料有所不同。本文给出了一个经验性的氮化物的Eh—pH曲线图,这个经验性的Eh—pH曲线图与地下水中氮化物的实际分布相一致。 相似文献
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Distribution of organic carbon in sediments and its influences on adjacent sea area in the turbidity maximum of Changjiang Estuary in China 总被引:2,自引:0,他引:2
Distributions and sources of total organic carbon (TOC)in seabed sediments and their implications for hydrodynamics are analyzed, in the turbidity maximum of the Changjiang Estuary. Ecology ecoenvironmental effects of estuary water on the continuously increasing terrigenous organic carbon from the Changjiang River are also explored through variations of organic carbon content and water quality indicators. Results show that, hydrodynamics exert important influences on distributions of organic carbon in the tur- bidity maximum of Changjiang Estuary. For their redistribution effect of terrigenous organic carbon within the moving layer in the whole region, variations from land to sea are not indicated by surficial and vertical average values of TOC and total nitrogen (TN) contents in core sediment, as well as organic stable carbon isotopes in surface sediments. However, on the long-time scale, the trend of terrigenous organic carbon decreasing from land to sea is still displayed by variations of stable carbon isotopic average values becoming heavier from land to sea. Previous studies have shown that high content of Chl a cannot appear in the Changjiang Estuary in despite of adequate nourishment supply, because photosynthesis of phytoplankton is constrained by high suspended sediment concentration(SSC). However, an area with a high content of Chl a occurs, which may be caused by resuspended benthic algae with bottom fine grain-size sediments. Tremendous pressures are imposed on the environment of Changjiang Estuary, because of uhrophication trends and special hydrodynamics. Phytoplankton bloom area tends to extend from the outer sea to the mouth of Changjiang River. 相似文献
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利用次网格技术模拟华东地区大气硫氮沉降 总被引:5,自引:1,他引:5
采用数值模拟方法,在区域酸性沉降模式系统中引入次网格处理技术。通过4种次网格方案模拟结果的相互比较,选择最优方案,然后利用最优次网格方案,选取华东地区为例,进一步模拟研究大气硫氮沉降的空间分布。结果表明,就干沉积速率而言,以细网格方案(水平分辨率25 km)为参照,采用次网格方案比粗网格方案(水平分辨率75 km)有明显改进,其中“次网格风速与摩擦速度之积为常数”为最优次网格方案。华东地区硫的年总沉降量是1.92 mt(1 mt=106ton),氮的年总沉降量是0.65mt。华东地区硫化物(SO2、硫酸盐SO42-)干沉降量占总沉降量的49%,氮化物(NO、NO2、硝酸盐NO3-)干沉降量占总沉降量的80%,可见干沉降在大气沉降中具有重要地位。华东地区总的大气硫、氮沉降量中,70%以上到达有植被覆盖的土壤生态系统,这将对农田、草地和森林的硫素和氮素平衡有重要影响。此外,华东部分地区的硫沉降已经超过了临界负荷,而氮沉降尚未出现超临界负荷的现象。 相似文献
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北京地区气溶胶PM2.5粒子浓度的相关因子及其估算模型 总被引:2,自引:0,他引:2
文中运用统计分析和气象统计预报的方法,使用北京白石桥小区的污染物观测资料和同期北京地区的气象观测资料,对影响大气污染的气象因子进行了综合分析,并分别建立了气溶胶PM2.5粒子浓度与气体污染物、气象要素场的两类统计相关拟合模型。发现气溶胶PM2.5粒子浓度与气体污染物浓度存在不同程度的相关性,且与气象条件亦存在显著的相关关系,此类时空变化及其量化估算模型具有一定实际应用价值。通过确定气象要素场和气溶胶浓度的关系可进一步研究不同地区的污染物输送和污染源扩散影响的问题。 相似文献
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通过以各类氮化物及部氮分析方法进行分析比较,选择了适合水利系统现有条件下切实可行的分析方法,并对分析方法的技术关键作了进一步探讨,以利于对水利系统监测数据进行质量管理,确保水持数据的准确性和可比性,以及对水体水质进行准确全面评价。 相似文献
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