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81.
DiMilla PA Nixon SW Oczkowski AJ Altabet MA McKinney RA 《Marine pollution bulletin》2011,62(4):672-680
When nutrients impact estuarine water quality, scientists and managers instinctively focus on quantifying and controlling land-based sources. However, in Greenwich Bay, RI, the estuary opens onto a larger and more intensively fertilized coastal water body (Narragansett Bay). Previous inventories of nitrogen (N) inputs to Greenwich Bay found that N inputs from Narragansett Bay exceeded those from the local watershed, suggesting that recent efforts to reduce local watershed N loads may have little effect on estuarine water quality. We used stable isotopes of N to characterize watershed and Narragansett Bay N sources as well as the composition of primary producers and consumers throughout Greenwich Bay. Results were consistent with previous assessments of the importance of N inputs to Greenwich Bay from Narragansett Bay. As multiple N sources contribute to estuarine water quality, effective management requires attention to individual sources commensurate with overall magnitude, regardless of the political complications that may entail. 相似文献
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新生代时期渤海中部的强烈沉降,是多种物理条件的共同作用结果,这些条件是由裂谷期和后裂谷期的深部过程产生成的.裂谷期在异常热地幔背景下的渤海地壳隆起、减薄、张裂,地幔热物质上升侵入地壳,莫霍界面位置升高,积累了重力势能;后裂谷期岩石圈(层)的冷却、收缩及下地壳的相变导致密度增大,加上巨厚沉积物的持续增生,使地壳处于重力不平衡状态,向下的垂直力远大于向上的浮托力,同时还有东部后退位移性板块边界和下地壳侧向流动的支持,使渤海中部成为下沉速率最快、沉降幅度最大的凹陷盆地.后裂谷期的早期的盆地下沉具有分散、局部性特征,表现为多个凹陷和凸起交替组合格局;晚期转变为大范围的整体沉降,显示重力均衡和补偿过程是从浅往深发展的.先存的郯庐断裂带对沉降的空间范围有局部边界控制性作用,其本身可能受到盆地发展的强烈改造影响.盆地的基本变形机制是上地壳的水平向脆性张破裂和垂直向或近垂直向的正断层-剪切破裂,地震震源机制解和大地震时的地表破裂表现的水平错动反映中、下地壳的走滑-平移型应力状态及相应的瞬间水平剪切破裂,它与上地壳残留的伸展、下沉相容并存于三维地壳体内. 相似文献
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本研究玄武岩类岩体的强度与变形性质,并运用岩体分类系统分析其脆性断裂效应,从而为玄武岩体脆性反应变化范围提供依据。虽然,各类玄武岩的物质组成和物理指标很分散,但其许多性质指标都在系数约为10的范围内,在常温和低围压下完整玄琥岩岩块的强度参数的典型值为;杨氏模量78±19GPa;泊松比0.25±0.05;抗拉强度-14.5±3.3MPa。 相似文献
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88.
de Oliveira-Costa A Tegmark M Gutiérrez CM Jones AW Davies RD Lasenby AN Rebolo R Watson RA 《The Astrophysical journal》1999,527(1):L9-L12
The recent discovery of dust-correlated diffuse microwave emission has prompted two rival explanations: free-free emission and spinning dust grains. We present new detections of this component at 10 and 15 GHz by the switched-beam Tenerife experiment. The data show a turnover in the spectrum and thereby support the spinning dust hypothesis. We also present a significant detection of synchrotron radiation at 10 GHz, which is useful for normalizing foreground contamination of cosmic microwave background experiments at high galactic latitudes. 相似文献
89.
Composition and distribution of organochlorine pesticide residues in surface sediments from the Wu-Shi River Estuary,Taiwan 总被引:23,自引:0,他引:23
The contamination of organochlorine pesticides (OCPs) in sediments from the Wu-Shi River estuary was investigated to evaluate the pollution potentials and distribution of OCPs in central Taiwan. A total of 19 sediment samples were collected at five sampling stations along the River estuary. The concentrations of OCPs were in the range of 0.99–14.5 ng/g-dry weight (dw) for ΣHCH (-, β-, γ-, δ-HCH), 0.46–13.4 ng/g-dw for Σcyclodiene and 0.53–11.4 ng/g-dw for ΣDDT (p,p′-DDD, p,p′-DDE, p,p′-DDT). The mean concentrations of ΣHCH, Σcyclodiene and ΣDDT were 3.79, 4.87 and 2.51 ng/g-dw, respectively. The total concentrations of OCPs correspond to 1.73–71.9 μg/g-OC when normalized to TOC contents. Among the organochlorine pesticides, endosulfan sulfate, β-HCH, and p,p′-DDD were the most dominant compounds in the sediments with the average concentrations of 1.97, 3.43 and 2.08 ng/g, respectively. Also, different contamination patterns among sampling seasons were observed. The measured concentrations of OCPs collected in spring were higher than those in autumn and winter. A linear relationship between sediment characteristics and OCP residues was also demonstrated. The results obtained in this study show that there still exist a variety of organochlorine pesticide residues in the sediments from the near shore of central Taiwan. 相似文献
90.
中、新生代全球尺度地质过程及其对自然环境的影响 总被引:1,自引:0,他引:1
中、新生代是地球岩石圈经历重大构造演化 ,最终形成现今地球面貌的时代。研究对中、新生代全球级环境变化有重大影响的地质作用过程 ,对从整体上把握和理解环境演变的规律和原因 ,最终实现对环境变化的预测有重要意义。中生代开始不久 ,位于赤道附近的联合古陆便解体分裂 ,全球大陆和大洋逐渐演变成现今的分布格局。与此相伴 ,地球的地形、地貌也发生了重大变化。中生代造山运动造就的山脉和其后由构造隆升形成的高原 ,也是影响全球气候的主要因素之一。中、新生代的多次大规模火山活动 ,造成气候、环境的快速变化 ,甚至导致大规模生物灭绝。在中白垩世期间 ,发生了一系列全球规模的构造运动现象 ,它们与地球深部的超地幔柱有关。文中也通过天体撞击作用探讨了地外因素对地球环境和生命演化的影响。 相似文献