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大沽河是青岛市重要的供水源之一,了解大沽河流域水循环的过程和机理有助于合理地利用大沽河流域水资源。为了研究大沽河流域地下水循环的规律,在大沽河李哥庄镇至胶东镇段研究区内采集了26个地下水样本和4个地表水样本,测定其氢、氧同位素及水化学成分,通过分析其变化特征初步判定地下水补给来源以及影响因素。对降水和地下水中的稳定同位素组成(δD,δ~(18)O)进行分析,结果表明大气降水是该区域地下水的主要来源。地下水及地表水的水化学结果表明研究区地下水类型多样,主要为HCO_3-Cl-SO_4-Ca-Na,Cl-SO_4-Na,Cl-HCO_3-SO_4-Na,HCO_3-Cl-SO_4-Na-Ca-Mg,Cl-Na五类;地表水受到强烈的蒸发浓缩作用,并在一定程度上补给了地下水。同时,地下水中的氢、氧同位素含量与Cl~-和TDS区域分布特征相互佐证,证明地下水化学成分主要受到海水入侵的影响,其次为围岩矿物的溶解。 相似文献
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双台子河口重金属污染的沉积记录 总被引:3,自引:0,他引:3
根据双台子河口沉积柱中微量金属的含量及沉积物的粒度参数,结合137Cs放射性比活度精确定年,研究了双台子河口的沉积速率和重金属的污染变化特征,并利用地累积指数法评价了重金属的污染程度。137Cs计年的结果表明,沉积柱的平均沉积速率为1.3cm/a。沉积物的粒径从底层向表层逐渐变细,反映了水动力条件的减弱。绝大多数重金属的含量基本上都是自底部向上逐渐增加。重金属元素与细粒沉积物(63μm)均具有较好的正相关性,说明细粒物质对重金属具有较高的吸附能力。采用地累积指数对沉积柱中重金属元素的垂向变化进行了评价,发现除Cd元素外,大部分元素均未受到污染(Igeo0)。推测Cd的污染可能主要与20世纪90年代起至今人类活动对双台子河口产生的影响逐渐增加有关。 相似文献
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基于卫星高度计的北极海冰厚度变化研究 总被引:2,自引:3,他引:2
A modified algorithm taking into account the first year(FY) and multiyear(MY) ice densities is used to derive a sea ice thickness from freeboard measurements acquired by satellite altimetry ICESat(2003–2008). Estimates agree with various independent in situ measurements within 0.21 m. Both the fall and winter campaigns see a dramatic extent retreat of thicker MY ice that survives at least one summer melting season. There were strong seasonal and interannual variabilities with regard to the mean thickness. Seasonal increases of 0.53 m for FY the ice and 0.29 m for the MY ice between the autumn and the winter ICESat campaigns, roughly 4–5 month separation, were found. Interannually, the significant MY ice thickness declines over the consecutive four ICESat winter campaigns(2005–2008) leads to a pronounced thickness drop of 0.8 m in MY sea ice zones. No clear trend was identified from the averaged thickness of thinner, FY ice that emerges in autumn and winter and melts in summer. Uncertainty estimates for our calculated thickness, caused by the standard deviations of multiple input parameters including freeboard, ice density, snow density, snow depth, show large errors more than 0.5 m in thicker MY ice zones and relatively small standard deviations under 0.5 m elsewhere. Moreover, a sensitivity analysis is implemented to determine the separate impact on the thickness estimate in the dependence of an individual input variable as mentioned above. The results show systematic bias of the estimated ice thickness appears to be mainly caused by the variations of freeboard as well as the ice density whereas the snow density and depth brings about relatively insignificant errors. 相似文献
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不同贮藏条件和光照对5种蒺藜科植物种子萌发的影响 总被引:6,自引:6,他引:6
研究不同贮藏条件和光照对5种蒺藜科植物(骆驼蓬 Pegannum harmala、唐古特白刺Nitrari tangutorum、泡泡刺Nitraria sphaerocarpa、驼蹄瓣 Zygophyllum fabago 和多裂骆驼蓬Peganum multisectum)种子萌发的影响。结果表明,低温贮藏对这5种植物的种子萌发有显著影响,并且种子萌发对光、暗的响应随贮藏条件和贮藏时间的变化而变化。根据这5种植物在不同条件组合下的最大萌发率,拟定出了种子萌发的最佳贮藏条件和萌发条件:①湿-冷贮藏能使骆驼蓬种子具有较高的萌发率,此时对光照没有明显的要求;②多裂骆驼蓬种子经过80 d湿-冷贮藏后在光下能达到很高的萌发率,同时,其80 d干-冷贮藏后在暗条件下的萌发率接近同样的效果;③唐古特白刺种子更适合光下萌发,在湿+低温+光照处理下,种子经过三个贮藏期后均具有较高的萌发率,而干-冷贮藏种子只有冷藏80 d后才能达到较高萌发率;④泡泡刺种子适合干-冷贮藏,对光照没有要求;⑤驼蹄瓣种子在干、湿贮藏后,其萌发率无明显差异,但在暗条件下萌发率略高于光条件下,并且达到最大萌发率所需要的冷藏时间短(20 d),而在光下则需要较长的冷藏(80 d 以上)才能达到较高萌发率。 相似文献
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北极地区不同冰龄的海冰厚度变化研究 总被引:1,自引:0,他引:1
In this study, changes in Arctic sea ice thickness for each ice age category were examined based on satellite observations and modelled results. Interannual changes obtained from Ice, Cloud, and Land Elevation Satellite(ICESat)-based results show a thickness reduction over perennial sea ice(ice that survives at least one melt season with an age of no less than 2 year) up to approximately 0.5–1.0 m and 0.6–0.8 m(depending on ice age) during the investigated winter and autumn ICESat periods, respectively. Pan-Arctic Ice Ocean Modeling and Assimilation System(PIOMAS)-based results provide a view of a continued thickness reduction over the past four decades. Compared to 1980 s, there is a clear thickness drop of roughly 0.50 m in 2010 s for perennial ice. This overall decrease in sea ice thickness can be in part attributed to the amplified warming climate in north latitudes. Besides, we figure out that strongly anomalous southerly summer surface winds may play an important role in prompting the thickness decline in perennial ice zone through transporting heat deposited in open water(primarily via albedo feedback) in Eurasian sector deep into a broader sea ice regime in central Arctic Ocean. This heat source is responsible for enhanced ice bottom melting, leading to further reduction in ice thickness. 相似文献
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