Benthic nutrient fluxes in the intertidal flat within the Changjiang （Yangtze River） Estuary   总被引：1，自引：0，他引：1  

GAO Lei    LI Daoji  WANG Yanming  YU Lihua  KONG Dingjiang  LI Mei  LI Yun  and FANG Tao State Key Laboratory of Marine Geology  Tongji University  Shanghai  China State Key Laboratory of Estuarine  Coastal Research  East China Normal University  Shanghai  China 《中国地球化学学报》2008,27(1):58-71

In an annual cycle from March 2005 to February 2006, benthic nutrient fluxes were measured monthly in the Dongtan intertidal flat within the Changjiang （Yangtze River） Estuary. Except for NH4^＋, there always showed high fluxes from overlying water into sediment for other four nutrients. Sediments in the high and middle marshes, covered with halophyte and consisting of macrofauna, demonstrated more capabilities of assimilating nutrients from overlying water than the low marsh. Sampling seasons and nutrient concentrations in the overlying water could both exert significant effects on these fluxes. Additionally, according to the model provided by previous study, denitrification rates, that utilizing NO3- transported from overlying water （Dw） in Dongtan sediments, were estimated to be from -16 to 193 μmol·h^-1·m^-2 with an average value of 63 μmol·h^-1·m^-2 （n=18）. These estimated values are still underestimates of the in-situ rates owing to the lack of consideration of DN, i.e., denitrification supported by the local NO3^- production via nitrification.  相似文献   

河南镇平秋树湾矿区铜、钼矿床地质特征及深部找矿潜力分析   总被引：7，自引：1，他引：6  

张智慧  秦明  方荣  唐杰  翟东旭 《矿产与地质》2008,22(2):107-110

秋树湾矿区是一座中型规模的铜、钼矿床。在水平方向上矿区具北铜南钼的分布特征,即北山铜矿床和南山钼矿床;从垂向上看,北山铜矿床深部赋存有规模较大的钼矿体,并具垂直分带现象,即上铜下钼。这主要是矿区成矿后,构造活动使南山赋矿区向上逆冲,使其上部的铜矿体被剥蚀,而北山赋矿区上部的矿体则保存了下来。因此,研究认为,在北山铜矿区的下部及南山钼矿区中深部寻找隐伏钼矿床具有较大潜力。  相似文献   

盆地地下水系统的数值模拟研究——以山西灵石静升盆地为例     

赵春虎  李国敏  黎明  肖永吉  樊荣 《地下水》2008,30(2):14-17

以山西灵石静升盆地为例,选择三维流数学模型,合理刻画了模型边界,利用CFC定年技术对模型进行识别校正,提高了模型仿真程度,构建了适合盆地地下水系统的数值模型.最后对不同水平年盆地水动力特征进行了输出分析.  相似文献   

中元古代晚期浅海高能沉积环境中的海绿石:以天津蓟县剖面铁岭组为例   总被引：7，自引：0，他引：7  

梅冥相  杨锋杰  高金汉  孟庆芬 《地学前缘》2008,15(4):146-158

海绿石是一种富钾、富铁的含水层状铝硅酸盐矿物,在沉积学领域常被作为一种普遍的指相矿物。多年研究的结果表明,现代海绿石主要形成在慢速、弱还原的较深水环境中,而且还可以作为"凝缩段"的识别标志之一。天津蓟县剖面中元古界铁岭组第二段灰岩中的海绿石,产在高能叠层石岩礁之中,主要以胶体形式富集在叠层石和均一石的边界上,代表较为典型的原地海绿石;较高的氧化钾含量(大于8%)而显示出高成熟海绿石的特点。很明显,铁岭组二段灰岩中的原地高成熟海绿石,不但不能作为"凝缩段"的识别标志,而且也不是长时间地层间断的产物。由于形成在正常高能浅海环境,而且处于中元古代末期,与现代沉积中的海绿石存在较大的差异,可能代表了中元古代末期的正常浅海还处于含氧量不够充分的弱还原状态,最终使铁岭组灰岩中的海绿石成为前寒武纪海绿石产出的一个典型代表,也间接的表明了在漫长的地质历史演变过程中海绿石产出的多样性特点。  相似文献   

临海市基本农田信息化建设及具体应用   总被引：2，自引：1，他引：1  

徐德军  钟美  杜清运 《地理空间信息》2008,6(3):35-37

分析了基本农田信息化建设的现状,提出了临海市基本农田信息化建设的总体框架。阐述了基本农田信息系统的建设,以及基本农田信息系统的具体作用。对于各地的基本农田信息化建设具有一定的借鉴意义和价值。  相似文献   

Sedimentary characteristics of terrigenous debris at site MD05-2905 in the northeastern part of the South China Sea since 36 ka and evolution of the East Asian monsoon     

Wenguang Yang  Hongbo Zheng  Ke Wang  Xin Xie  Guocheng Chen  Xi Mei 《Frontiers of Earth Science》2008,2(2):170-176

Sediments with high sedimentation rate at site MD05-2905 in the Northeastern slope of the South China Sea provide unique materials for a high-resolution study on the paleoenvironment. Based on precise dating of AMS ¹⁴C, grain size analysis of terrigenous debris at core MD05-2905 was conducted after organic matter, biological carbonate and biogenic opal were removed. The results show that 15.5–63.5 μm coarse grain size ingredients may indicate East Asian winter monsoon changes and that 2–9 μm fine grain size ingredients may be used as a proxy of evolution of the East Asian summer monsoon. The results of grain size analysis, which suggest East Asian monsoon intensity, reveal that a winter monsoon dominated the glacial regime and a summer monsoon dominated the Holocene regime. It was also shown that the summer monsoon increased gradually, experienced several abrupt changes and reached a culmination in the early Holocene (11200–8500 a B.P.) since 36 ka. Controlled by precession periodicity, it may be related with the amount of solar radiation at the highest stage, which needs further study. __________ Translated from Advances in Earth Science, 2007, 22(10): 1012–1018 [译自: 地球科学进展]  相似文献   

Densities of Huanghe River estuary and Bohai Bay waters     

陈国华  季荣  谢式南  张力军 《中国海洋湖沼学报》1994,12(2):130-135

The densities of 36 water samples from the Huanghe River estuary and Bohai Bay were determinedby a magnetic float densimcter under three temperatures from 15℃ to 25℃.All the measured densities ofsamples were greater than that of the values calculated from the International Equation of State of Seawater.The differences between the measured and calculated densities increased with the decrease of salinities.The dif-ferences appeared exponentially correlated with[Ca~(2+)]/s,[Mg~(2+)]/s and[SO_4~(2-)]/s,and had"s"type curverelationship with the alkalinity in all salinity range.But in the salinity ranging from 25.72 to 31.57,therelationships were all linear.The density difference can be estimated from the equation △ρ（10~3kg·m~(-3)）=（-2.79+236.5([Ca~(2+)]/s)/(-9.7464×10~（-3）+[Ca~(2+)]/s).It was the high alkalinity and[Ca~(2+)]/s that resulted in the measured densi-ties of seawaters being higher than the calculated densities in the Huanghe estuary and Bohai Bay.  相似文献   

普里兹湾邻近海域大磷虾的生殖特点研究          下载免费PDF全文

王荣  张云波  仲学锋  孙松  柳满然 《极地研究》1993,5(4):12-21

本文依据 1 989/1 990和 1 990 /1 991夏季 ,“极地”号考察船在普里兹湾邻近海域 (南大洋的印度洋区 )的拖网样品 ,对大磷虾的性腺发育和生殖群体的年龄结构等 ,进行了分析研究。大磷虾的生殖开始于 1月 ,一直持续到 3月。高峰期出现在 2月中旬 ,比大西洋区相比迟了一个月。生殖群体主要包括两个年龄组 ,即 3 + 龄和 4+ 龄。换句话说 ,绝大部分个体是三年性成熟 ,一生可生殖两次 ,不排除少数个体两年性成熟 ,或第三次性成熟的可能 ,但比例非常小。在 5 91 6尾能区分性别的个体中 ,雄性个体只占 3 4 .1 %。雄性比随体长的增加而降低。体长大于 5 0 mm的个体中雄性仅占 2 2 .9%。  相似文献   

高原大地形及海洋热力强迫对东亚及北半球环流和气候变化影响的观测研究     

罗会邦  陈蓉 《气象科学》1995,15(4):17-29

本文总结了“青藏高原大地形及西太平洋暖池势力强迫对东亚及全球气候变化的影响”专题五年来的主要研究工作。其中包括青世故高原东部大气热源的时间演变特征,夏半年高原热源异常对我国降水和北半球环流的影响;西沙海温变化特征及其与我南方降水的关系,北太平洋海温主因子特征及其与华南前汛期降水的变化。  相似文献   

Adsorption of aluminium by a latosol as affected by phosphate and glutamic acid     

Jie Wen Yang  Rong Fa Guo  Sheng Qi Chen 《Environmental Geology》2006,50(6):867-871

The effect of phosphate and glutamic acid on adsorption of aluminium onto a latosol was investigated as a function of pH and ligand concentrations through batch equilibrium experiments. The results showed that adsorption of aluminium by the soil was enhanced after addition of phosphate at low pH, and this promotive effect was gradually eliminated with the increase in pH. The positive effect of phosphate on aluminium adsorption onto latosol was attributed to phosphate-induced surface negative charge and formation of ternary surface complexes involving aluminium and phosphate. While using silica as adsorbent, the inactive surfaces for phosphate, promotion of adsorption of aluminium by phosphate was also found. Then it was proposed that additional aluminium might bind to the phosphate adsorbed onto the silica in the form of surface complexes silica–aluminium–phosphate again, and the mechanism might operate in the soil systems as well. Glutamic acid exhibited no influence on the adsorption of aluminium by the soil at low pH. After increasing the pH, adsorption of aluminium was inhibited especially with the highest addition of glutamic acid, probably owing to weak affinity of complexes between glutamic acid and aluminium to the soil.  相似文献