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971.
在靖边油区油井施工中,白垩系下统洛河组砂岩底部泥浆漏失概率42%~66%,而砂岩其它部位未出现漏水现象。侏罗系中统安定组与上覆洛河组呈角度不整合接触,古风化壳的存在使安定组顶部灰岩裂隙十分发育,最大漏失量达0.88m3/mm。故洛河组砂岩底部与安定组泥灰岩是靖边油区开发地下水的较佳部位。 相似文献
972.
通过2000年和2001年的试验研究,证明我区气候是适宜瓜尔豆生长的,并进一步研究出瓜尔豆正常生长所需的气象指标。 相似文献
973.
974.
1 IntroductionThe drainage network is one of the important components in a fluvial system, as Schumm[1] pointed out that three zones compose a typical fluvial system. As early as in the mid 20th century, Horton[2] made a significant quantitative explanation to hydro-geomorphology in a drainage network system. Since the 1960s, Leopold and Langbein have studied the network structure with random walk and entropy, and Shreve, Smart and Scheideger have topologically studied network structure[3-1… 相似文献
975.
976.
Bent Vad Odgaard 《Journal of Paleolimnology》1993,8(1):3-13
Sediment distribution was mapped by multiple corings in a small oligotrophic lake in northwestern Denmark. Sediment cores along a representative West-East transect were dated by 14C and correlated using pollen, mineral magnetics and general lithology. Estimates of whole-lake Holocene sediment accumulation were used to calculate sediment yield (terrestrial erosion). Results indicate that: 1) sediment yield was low 10000–5000 BP and increased strongly 5000–2500 BP and again 2500–1200 BP, 2) sediment focusing and waves and currents induced by strong winds were the major processes controlling sediment distribution throughout the Holocene; 3) the dominant wind direction of strong winds has been westerly throughout the Holocene; and 4) the lake was probably more productive in the last 5000 years than in the period from 10000 to 5000 BP. 相似文献
977.
978.
In contrast to much previous research on blanket peat moorland, which has concentrated upon studies of the form and causes of gully erosion, this paper attempts to investigate sediment transport and to estimate both short-term and long-term sediment yields in such terrain. The research was conducted on Wessenden Head Moor to the west of Huddersfield, Yorkshire, where automatic stream sampling continued over a period of two years. Use of corrected rating curves (Ferguson, 1988) provided a mean estimate of sediment yield over this period of 55 t km?2 yr?1. In addition an estimate of longer-term sediment yield was derived from four reservoir sediment surveys in the Wessenden Valley. Total yield was 203.69 t km?2 yr?1, including an organic fraction of 38.82 t km ?2 yr?1. Stream sampling at three sites on Shiny Brook, including headwaters and the outflow to the reservoir, suggested that there is great temporal and spatial variability in mineral and organic inputs to the reservoirs. Although not excessive in gravimetric terms, the low density of peat means that there is a serious erosion problem. Estimates of erosion rates for the peat gully network at Shiny Brook appear to confirm earlier evidence concerning the relatively recent occurrence of this erosion, within the last two centuries. 相似文献
979.
EFFECTOFFINEPARTICLESONTHEVERTICALCONCENTRATIONDISTRIBUTIONANDTRANSPORTRATEOFCOARSEPARTICLESWANZhaohui;SONGTianchengAbstract:... 相似文献
980.
简要介绍了三个国内常用的水文模型,探讨了这三个模型中的蒸发、下渗、产汇流机制,并剖析了模型中存在的问题. 相似文献