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41.
流动重力观测结果显示,地震孕育过程中重力变化最大处往往不与震中重合,美国科学家J.T.Kuo(郭宗汾)提出了孕震体质量变化中心震质源(hypocentroid)和其在地表的投影震质中(epicentroid)的概念.本文采用球、椭球和圆柱体等3种旋转体模型模拟孕震体,分别计算孕震体均匀膨胀引起的表面重力变化模型,并利用最小二乘法对1981~2000年发生在京津唐张测网内16次M>4.0地震进行震质中迭代反演. 计算精度表明,圆柱体模型为三者中的最隹模型.研究了震中、震质中与断层之间的位置关系,发现京津唐张地区M4~5地震震质中与震中的距离在0~40 km之间,震中一般发生在断层末端,或断层交汇处;而震质中大都发生在断层间的块体内,且成丛分布.这意味着区域内存在小范围的构造——地震孵化区,一次次地震在孵化区内孵化,但却在其周围发生.其间,断层的存在起着重要的控制作用. 相似文献
42.
Joanna K. York Gabrielle Tomasky Ivan Valiela Anne E. Giblin 《Estuaries and Coasts》2010,33(5):1069-1079
We measured fluxes of NH4+ and NO3− and δ15N of NH4+, sediment, and porewater NH4+ from incubated sediment cores along a nitrate gradient and in different seasons from Childs River, MA. NH4+ flux was low at the downstream site with the lowest concentration of organic matter (high salinity) but otherwise did not
differ along the estuary. The δ15N of regenerated NH4+ ranged from +6.1‰ to +15.3‰ but did not vary significantly with season or salinity; the mean for the entire estuary was +10.4 ± 0.5‰.
Based on differences between the δ15N of regenerated NH4+ and sediment, and expected isotopic fractionation due to remineralization, we concluded that nitrification occurred after
remineralization of NH4+. Differences between the δ15N of regenerated NH4+ and the δ15N of porewater NH4+ provided further evidence of nitrification. We estimated that 11% to 48% of remineralized NH4+ underwent coupled nitrification–denitrification before release into the water column. In spite of losses to denitrification,
NH4+ flux released 1.4 mol N m−2 year−1 to the water column and could provide 42% of phytoplankton nitrogen requirements. 相似文献