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91.
This paper examines the potential role of forest set-asides in global carbon sequestration policy. While set asides that protect
forests from timber harvests and land-use conversion may alleviate concerns with permanence, and they may provide large ancillary
environmental benefits, they may also lead to large leakage. This paper uses a global land use and forestry model to examine
the efficiency of three crediting schemes for set-asides. The results show that if set-asides are integrated into a global
forestry carbon sequestration program that includes a wide range of other management options, then 300 million hectares of
land would be set-aside, and up to 128 Pg C could be sequestered in global forests by 2105. Under alternative policies that
focus exclusively on set-asides, more forestland can be set-asides, up to 3.2 billion hectare, but these policies invite large
leakage in the near-term, and in the long-run, they less net carbon is removed from the atmosphere. Specifically, leakage
is estimated to be 47–52%, depending on the policy, and by the end of the century, up to 17% less carbon will be sequestered
in all forests. 相似文献
92.
Jiamo Fu Guoying Sheng Deyu Chen Dehan Liu S. C. Brassell A. Gowar G. Eglinton 《中国地球化学学报》1987,6(4):289-296
A preliminary study of newly discovered sphagnum brown coal from the Jingsuo Basin, Yunnan Province, China, which is quite
rich in montan wax, indicates the predominance of highern-alkane homologues and aromatized triterpenoid components. Aromatic hydrocarbons are composed mainly of pentacyclic and tetracyclic
di-, tri- and tetra-aromatic components, which are obviously diagenetically related to higher plant-derived triterpenoids
naturally occurring in the biosphere. Because the sphagnum brown coal still remains in the highly immature stage, it seems
that the progressive diagenetic aromatization of the higher plant-derived triterpenoids may start at a very early stage. 相似文献
93.
The combination of magnetotelluric survey and laboratory measurements of electrical conductivity is a powerful approach for exploring the conditions of Earth’s deep interior. Electrical conductivity of hydrous silicate melts and aqueous fluids is sensitive to composition, temperature, and pressure, making it useful for understanding partial melting and fluid activity at great depths. This study presents a review on the experimental studies of electrical conductivity of silicate melts and aqueous fluids, and introduces some important applications of experimental results. For silicate melts, electrical conductivity increases with increasing temperature but decreases with pressure. With a similar Na+ concentration, along the calc-alkaline series electrical conductivity generally increases from basaltic to rhyolitic melt, accompanied by a decreasing activation enthalpy. Electrical conductivity of silicate melts is strongly enhanced with the incorporation of water due to promoted cation mobility. For aqueous fluids, research is focused on dilute electrolyte solutions. Electrical conductivity typically first increases and then decreases with increasing temperature, and increases with pressure before approaching a plateau value. The dissociation constant of electrolyte can be derived from conductivity data. To develop generally applicable quantitative models of electrical conductivity of melt/fluid addressing the dependences on temperature, pressure, and composition, it requires more electrical conductivity measurements of representative systems to be implemented in an extensive P-T range using up-to-date methods. 相似文献
94.
Kapil Bisht Yogesh Joshi Shashi Upadhyay Poonam Metha 《Journal of the Geological Society of India》2018,92(2):173-176
Glaciers being very sensitive to climate change have been identified as one of the best indicators of climate change and evidences have proved that most of the Himalayan glaciers have receded with an increased rate during the recent past under the influence of global warming. Lichenometric study was carried out on the moraines of Milam glacier (located in Pithoragarh district of Uttarakhand) with the help of lichen species Dimelaena oreina having an average annual growth rate of 1.31 mm. The study revealed that Milam glacier has receded 1450 m in last 69.37 years with an average recession rate of 20.90 m/year. Since lichenometric studies are cost effective and ecofriendly in comparison to carbon dating, satellite and remote sensing based studies and also reliable, hence, it should be promoted in Himalaya which is an abode of glaciers. 相似文献
95.
我国地质分析综述论文统计 总被引:2,自引:0,他引:2
作者检索了地质分析专业刊物《岩矿测试》、《地质实验室》全部论文以及国内相关期刊近30年来的文献.统计分析了地质分析综述性文献在各有关期刊的分布及特点,为了解和评价国内地质分析文献的基本状况提供了有益信息。 相似文献
97.
利用EQIM软件建设和拓展广西地震速报系统 总被引:1,自引:0,他引:1
介绍在全国EQIM软件基础上,结合广西地震台网速报工作的需要,开发适用于广西区域台网内部使用的广西地震速报系统,其基本功能包括:地震速报、信息共享、手机短信发布、Web互联网查询数据资料、数据汇集等多个方面.广西地震速报系统的建立可提高地震速报信息向各级部门的快速传递能力,并为分析预报人员提供及时的地震数据服务. 相似文献
98.
非线性参数H值用于华北地区的预报方案研究及检验 总被引:2,自引:0,他引:2
陈佩燕 《地震地磁观测与研究》1996,17(1):76-80
本文研究了非线性参数H值曲线与华北强震之间的关系。将RSH算法应用于华北地区,研究了定量预报指标的方案,并进行了回溯性预报检验。 相似文献
99.
Prabhin Sukumaran Dhananjay A. Sant K. Krishnan Govindan Rangarajan 《Journal of the Geological Society of India》2012,79(1):41-52
A high resolution quantitative granulometric record for site Uchediya [21°43′2.22″ N, 73° 6′26.22″ E; 10 m a. s. l.] gives
understanding towards accretion history of the late Holocene flood plain in the lower reaches of Narmada River. Two sediment
facies (sandy and muddy) and seven subfacies (sandy subfacies: StMS+FS+CS, SmFS+MS, SlFS+VFS, and StMS + CS; muddy subfacies: FmSILT+VFS+FS, FmSILT+VFS (O) and FmSILT+VFS (T)) are identified based on cluster analysis supplemented with sedimentary structures observed in field and other laboratory
data. Changes in hydrodynamics are further deduced based on various sedimentological parameters and their ratios leading to
arrive at a depositional model. 相似文献
100.
Tamás Mikes Dominik Christ Rüdiger Petri István Dunkl Dirk Frei Mária Báldi-Beke Joachim Reitner Klaus Wemmer Hazim Hrvatović Hilmar von Eynatten 《Swiss Journal of Geoscience》2008,101(1):31-54
Sandwiched between the Adriatic Carbonate Platform and the Dinaride Ophiolite Zone, the Bosnian Flysch forms a c. 3000 m thick, intensely folded stack of Upper Jurassic to Cretaceous mixed carbonate and siliciclastic sediments in the Dinarides. New petrographic, heavy mineral, zircon U/Pb and fission-track data as well as biostratigraphic evidence allow us to reconstruct the palaeogeology of the source areas of the Bosnian Flysch basin in late Mesozoic times. Middle Jurassic intraoceanic subduction of the Neotethys was shortly followed by exhumation of the overriding oceanic plate. Trench sedimentation was controlled by a dual sediment supply from the sub-ophiolitic high-grade metamorphic soles and from the distal continental margin of the Adriatic plate. Following obduction onto Adria, from the Jurassic–Cretaceous transition onwards a vast clastic wedge (Vranduk Formation) was developed in front of the leading edge, fed by continental basement units of Adria that experienced Early Cretaceous synsedimentary cooling, by the overlying ophiolitic thrust sheets and by redeposited elements of coeval Urgonian facies reefs grown on the thrust wedge complex. Following mid-Cretaceous deformation and thermal overprint of the Vranduk Formation, the depozone migrated further towards SW and received increasing amounts of redeposited carbonate detritus released from the Adriatic Carbonate Platform margin (Ugar Formation). Subordinate siliciclastic source components indicate changing source rocks on the upper plate, with ophiolites becoming subordinate. The zone of the continental basement previously affected by the Late Jurassic–Early Cretaceous thermal imprint has been removed; instead, the basement mostly supplied detritus with a wide range of pre-Jurassic cooling ages. However, a c. 80 Ma, largely synsedimentary cooling event is also recorded by the Ugar Formation, that contrasts the predominantly Early Cretaceous cooling of the Adriatic basement and suggests, at least locally, a fast exhumation. 相似文献