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61.
在对河流游憩概念认识、发展背景和研究进展进行分析的基础上,从资源保护的视角出发,对河流游憩规划的本质和国外规划实践中所面临的基本问题及其解决方法进行深入探讨,认为游憩利用和保护的关系协调、游憩和其他河流利用的关系协调、游憩利用本身所面临的问题是河流游憩规划需要解决的基本问题,得出保护性利用是河流游憩规划主旋律的结论。 相似文献
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不同土地利用方式下渭-库绿洲土壤盐渍化特征分析 总被引:4,自引:0,他引:4
基于渭干河—库车河三角洲绿洲土壤盐渍化现象发展的趋势,采用经典统计分析方法,对研究区不同土地利用方式下的土壤电导率、总盐量和pH值进行描述性统计分析,通过单因素方差方法对不同土地利用方式下土壤盐分指标进行差异显著性检验,并利用最小显著极差法(LSD)进行多重比较。研究结果表明:在不同土地利用方式和土层深度下,土壤电导率和总盐量的平均水平差异显著(p0.05),其含量由高到低依次为:荒漠灌丛盐碱草地耕地林地,而土壤pH值则无显著差异,土壤盐分呈现出明显的表层富集现象。本研究的结论对于提高此区域农业生产潜力和盐碱地综合治理具有重要的理论和实际意义。 相似文献
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Background, Aim and Scope The distribution of sediments in estuarine beaches is controlled by the interactions between sediment supply, hydrodynamic
processes and human intervention. The main purpose of this study is to characterize the sediments of Tagus estuarine beaches
in order to understand their origin and to contribute to a better knowledge of the Tagus estuary sediment budget.
Methods Surface sediment samples were collected across beach profiles and sand grain size analysis was performed by dry sieving. Grain
size statistics for the median (d50) and standard deviation (SDM) were obtained using the Moment method. This study was complemented by a qualitative evaluation
of the sediment composition. Cross-shore topographic surveys were conducted for selected sampling sites.
Results Tagus estuarine beach sediments are mainly composed of quartz sand particles which are fine-grained and well sorted near the
mouth of the estuary and medium to coarse-grained and moderately sorted in the inner domain. Compositional results show evidence
of active anthropogenic sediment sources, especially in the coarser fractions.
Discussion The analysis of the textural and compositional characteristics of beach sediments in the inner estuarine domain is compatible
with local sedimentary sources, while a marine signature is present at the mouth and inlet channel sediments. In the inner
domain, differences in the sedimentary processes are represented by the textural characteristics of the sediments, such as
the sorting degree and the gravel content. Sediment characteristics also reflect human intervention in the system, with the
introduction of anthropogenic and allochthonous particles and the mixture of sediments from different sources.
Conclusions The sediments of the inner Tagus estuarine beaches are derived from local Plio-Pleistocene outcrops while inlet and outer
estuary beaches reveal a dominant marine source. Beach textural variability observed in the inner domain is not related to
wave forcing gradients, but mainly to variations in the sedimentary processes along the estuarine margins and to human intervention.
Results show that the Tagus estuarine beaches depended, almost exclusively, on sediment input from local sources until the
last century. With increasing human occupation, sediment transfers became dominated by anthropogenically related activities
mainly connected with the occupation of estuarine margins and dredging.
Recommendations and Perspectives Further studies should extend the present level of knowledge in what concerns sand transport patterns through additional compositional
and geochemical analysis, and the development of new techniques in order to allow the quantitative evaluation of the impact
of human activities on the sediment budget. 相似文献
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Presently, the soil water balance of flood‐influenced soils in fluvial plains is insufficiently described. The new development of a weighable groundwater lysimeter is the basis for recording the water‐balance components precipitation, evapotranspiration, groundwater recharge, capillary rise, and interaction with the water course. Soil‐hydrologic measuring setups at two floodplain sites of the Elbe river serve for direct comparability of lysimeter measurements with data obtained on site. A groundwater control was designed for lysimeters that automatically adjusts the current groundwater level at the floodplain measuring setups and quantifies inflow into or outflow from the lysimeter. It turned out that the lysimeter developed is capable of identifying the individual water‐balance quantities at high accuracy. Contrary to previous assumptions, it was possible to prove groundwater recharge for the floodplain sites. 相似文献
67.
清涧河流域水土流失严重。年侵蚀模数在10000t/km2以上。自50年代初开展水土保持工作,截至1989年底止,共治理水土流失面积2204.07km2,治理程度达50.67%,流域输水输沙明显减少。分析表明:清涧河水沙减少受降雨和流域治理的共同影响,与1969年以前相比,70年代年均减沙15.4%,80年代年均减沙71.3%。在减沙量中,降雨偏枯影响70年代占14.6%~28.2%,80年代占36.9%~41.8%;流域治理减沙量70年代占71.8%~85.5%,80年代占58.2%~63.1%。同时,流域治理减水量也由70年代的18.2%~33.9%增加到80年代的42.9%~47.7%。 相似文献
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Synthetic chelating agents such as EDTA form strong complexes with heavy metals and therefore have the potential to remobilize metals from sediments and aquifers. In natural waters EDTA is present almost exclusively in the form of metal-complexes. Therefore, remobilization of metals is always a metal-metal-EDTA exchange reaction. We have investigated, to our knowledge for the first time, the remobilization of metals from the surface of synthetic iron oxides and from a river sediment by different metal-EDTA complexes. The metals are exchanged as follows:MeEDTAdissolved + Meast
adsorbed MeastEDTAdissolved + Meadsorbed
The order of the remobilization rate of Zn2+ from goethite is CaEDTA > Fe(III)EDTA, reflecting the slow exchange reaction of Fe(III)EDTA. For the remobilization of Pb2+ from goethite, the rate was found to be Fe(III)EDTA > CaEDTA > ZnEDTA. Here, Fe(III)EDTA has surprisingly the fastest exchange rate. Only very limited remobilization of Pb2+ is possible from hydrous ferric oxide at pH 8 due to the very strong adsorption of Pb2+. The order of remobilization of Zn2+ from a natural river sediment was found to be CaEDTA > CuEDTA > Fe(III)EDTA. The remobilization rate of Zn2+ with Fe(III)EDTA is only 12% of the rate with CaEDTA, illustrating the importance of EDTA speciation for assessing remobilization. 相似文献