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661.
云南白垩系分布在滇中、滇西和澜沧江以西三个地域,彼此之间被深断裂所,它们的地质历程、构造特征各不相同。不能将澜沧江以西勐海、潞西地区的白垩系解体归属不同地层区。澜沧江以西的白垩系,分布于冈瓦纳古陆和古特提斯造带的小型山间盆地,地层层序齐全,岩性、厚度稳定,今古生物化石。有两套岩石序列,三个沉积旋回。 相似文献
662.
The main objectives of this study were to describe the seasonal standing stock dynamics of phytoplankton, bacterioplankton and heterotrophic flagellates in the highly eutrophic River Elbe (Germany), and to compare the seasonal patterns observed with other streams. Emphasis was placed on examining and assessing abiotic and biotic controlling factors influencing the structure and dynamics of the riverine plankton. All the physico-chemical and biological parameters determined were within the range or somewhat higher (in the case of phytoplankton abundance and biomass) than reported for other large streams. The underwater light conditions resulting from atypically short phytoplankton growth periods of about 6 months per year and the low phytoplankton carbon to chl a ratio of 23 were identified as a major limiting factor for phytoplankton development in the River Elbe. The seasonal distribution pattern of bacterioplankton indicated probable tight trophodynamical coupling both with phytoplankton and with heterotrophic flagellates, whereas heterotrophic flagellates showed a more trophic link with bacterial densities. Although approximately constant DOC and DON levels throughout the year sustained bacterial growth rates, during the phytoplankton growing season an increase of bacterial standing stocks was observed. Although the left-bank sampling site of the Elbe is strongly influenced by the tributaries Mulde and Saale containing higher concentrations of chloride, nitrogen nutrients, heavy metals and organic pollutants, no clear differences were observed between the two sides of the river concerning the biological parameters measured. Possible reasons and the slightly higher phytoplankton abundance and diversity at the right bank are discussed. 相似文献
663.
For data treatment of phytoplankton countings in the Lower Rhine the specific biovolume was calculated. The used computer-aided method is described, and the correlation between phytoplankton biomass, cell number and chlorophyll a is presented. 相似文献
664.
River incision and vegetation dynamics in cut-off channels 总被引:1,自引:0,他引:1
Gudrun Bornette Claude Amoros Jean-Claude Rostan 《Aquatic Sciences - Research Across Boundaries》1996,58(1):31-51
The consequences of river incision on ecosystems dynamics in cut-off channels were hypothesized to be 1) the reduction of river backflows and overflows of the river in the former channels; 2) the reduction of seepage flows from the river and drainage into the channels; 3) the drainage of the hillslope aquifer by the former channels. The subsequent changes of aquatic plant communities should be 1) the terrestrialization of the higher part of former channels and 2) their change into more oligotraphent ones if the hillslope aquifer is poorer in nutrients than the river. In those reaches where the river bed is aggraded, river backflows in the cut-off channel should increase, as should overflows and seepage, and more eutraphent species should develop. Changes in aquatic vegetation were studied over a ten-year period in four cut-off channels supplied by a nutrient-poor hillslope aquifer and a nutrient-rich river. Two of them were located in an incised reach of the river, one in an aggraded reach and one (reference) in a reach that was neither aggraded nor incised. The vegetation of the reference channel exhibited only minor changes over the ten-year period, indicating that the successional trend is not perceptible at the time scale of the study, and thus that any change observed in the other channels can be ascribed to river incision or aggradation. Terrestrialization expected in the channels located in the incised reach clearly progressed in the downstream parts, but was inhibited by groundwater supplies in the upper parts. As expected, oligotraphent communities progressed or remained dominant in the upper part. The channel located in the aggraded reach of the river exhibited the highest floristic changes. As expected, eutraphent communities progressed in this channel, but unexpectedly, terrestrialization also progressed in the upstream part. Alternative explanations are: 1) aggradation could have instigated more backflows and overflows without modifying significantly the mean water-level and 2) more frequent water overflows could have favoured alluvial deposition and thus terrestrialization. 相似文献
665.
The binding forms of Cd to an anaerobic sediment of low sulfide content from Lauffen reservoir (River Neckar, Germany) were studied using two different approaches, i. e. sequential extraction (modified from published protocols) and titrimetric study of the pH-dependent Cd release. Thermodynamic equilibrium calculations were applied to calculate both the release pattern of Cd during the titrations and the speciation of Cd within the single fractions of the extraction protocol. The calculations were based on measured sediment parameters such as hydrous ferric oxide (HFO), acid volatile sulfide, carbonate content and total Cd content, and the extractants (oxalate, acid etc.) used. The results of the two independent approaches coincided well in that they both assigned more than two thirds of the total Cd content to be adsorbed to organic matter. Cd bound as CdS is of little importance. Sequential extraction after a 3-month oxidation period at pH 7 revealed a shift of Cd from being mainly bound in stronger surface complexes with organic matter to being mainly bound in weaker surface complexes with organic matter and HFO, and thus becoming more bioavailable. This study suggests that the use of sequential extraction although being frequently criticized due to its operational character can be used to determine binding forms of metal ions if they are accompanied by 1) careful supporting experiments, 2) analysis of important sediment parameters, and 3) the use of thermodynamic equlibrium models which can help to understand Cd speciation within the extraction fractions. 相似文献
666.
新疆头屯河流域水沙特性与减沙治理 总被引:2,自引:0,他引:2
本文通过对头屯河流域山区各水文实测水文,泥沙资料的分析比较,揭示了头屯河水沙运移规律,指出了头屯河上游产水,中游产沙,水沙异源的特点,进而地实才考察测量的基础上,结合流域自然特点,提出了工程,生物措施相结合的减沙治理方案和在流域不同地段的具本治理措施。 相似文献
667.
塔里木河流域基础信息管理系统利用GIS技术、多媒体技术、DBMS技术,通过人-机交互地图控制方式提供数字地图、遥感数据、图形数据、属性数据、图像、声音、文字的输入、存贮、检索、分析和制图,实现了流域基础信息资源的现代化管理。 相似文献
668.
前汛期北江洪水过程水汽汇与河水流量的关系 总被引:4,自引:0,他引:4
本文分析了1980-1984年4-6月和1994年6月洪水过程北江流域的大气水汽汇特征及其与河水流量的关系。结果表明:前汛期洪水过程的前期大乞一般连续存在超过一定值的较强水汽汇,时间为1周左右,洪水的发生是强水汽汇连续产生的径流的积累所致;北江流域洪水期水汽汇的极大峰一般比石角站的洪峰流量超前2天左右,本文结果为洪水的预报提供一条新思路。 相似文献
669.
670.