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新研究表明岩浆来源深度比之前认为的更深 快报文章
地球科学快报,2022年第22期
作者:  王晓晨
Microsoft Word(14Kb)  |  收藏  |  浏览/下载:718/0  |  提交时间:2022/11/25
continental flood basalt  Heavy Rare earth elements  
Potential for large-scale CO2 removal via enhanced rock weathering with croplands 期刊论文
NATURE, 2020, 583 (7815) : 242-+
作者:  David J. Beerling;  Euripides P. Kantzas;  Mark R. Lomas;  Peter Wade;  Rafael M. Eufrasio;  Phil Renforth;  Binoy Sarkar;  M. Grace Andrews;  Rachael H. James;  Christopher R. Pearce;  Jean-Francois Mercure;  Hector Pollitt;  Philip B. Holden;  Neil R. Edwards;  Madhu Khanna;  Lenny Koh;  Shaun Quegan;  Nick F. Pidgeon;  Ivan A. Janssens;  James Hansen;  Steven A. Banwart
收藏  |  浏览/下载:56/0  |  提交时间:2020/07/14

Enhanced silicate rock weathering (ERW), deployable with croplands, has potential use for atmospheric carbon dioxide (CO2) removal (CDR), which is now necessary to mitigate anthropogenic climate change(1). ERW also has possible co-benefits for improved food and soil security, and reduced ocean acidification(2-4). Here we use an integrated performance modelling approach to make an initial techno-economic assessment for 2050, quantifying how CDR potential and costs vary among nations in relation to business-as-usual energy policies and policies consistent with limiting future warming to 2 degrees Celsius(5). China, India, the USA and Brazil have great potential to help achieve average global CDR goals of 0.5 to 2gigatonnes of carbon dioxide (CO2) per year with extraction costs of approximately US$80-180 per tonne of CO2. These goals and costs are robust, regardless of future energy policies. Deployment within existing croplands offers opportunities to align agriculture and climate policy. However, success will depend upon overcoming political and social inertia to develop regulatory and incentive frameworks. We discuss the challenges and opportunities of ERW deployment, including the potential for excess industrial silicate materials (basalt mine overburden, concrete, and iron and steel slag) to obviate the need for new mining, as well as uncertainties in soil weathering rates and land-ocean transfer of weathered products.


  
Hydrothermal (NN)-N-15-N-15 abundances constrain the origins of mantle nitrogen 期刊论文
NATURE, 2020, 580 (7803) : 367-+
作者:  Zhao, Steven;  Jang, Cholsoon;  Liu, Joyce;  Uehara, Kahealani;  Gilbert, Michael;  Izzo, Luke;  Zeng, Xianfeng;  Trefely, Sophie;  Fernandez, Sully;  Carrer, Alessandro;  Miller, Katelyn D.;  Schug, Zachary T.;  Snyder, Nathaniel W.;  Gade, Terence P.;  Titchenell, Paul M.;  Rabinowitz, Joshua D.;  Wellen, Kathryn E.
收藏  |  浏览/下载:34/0  |  提交时间:2020/05/13

Nitrogen is the main constituent of the Earth'  s atmosphere, but its provenance in the Earth'  s mantle remains uncertain. The relative contribution of primordial nitrogen inherited during the Earth'  s accretion versus that subducted from the Earth'  s surface is unclear(1-6). Here we show that the mantle may have retained remnants of such primordial nitrogen. We use the rare (NN)-N-15-N-15 isotopologue of N-2 as a new tracer of air contamination in volcanic gas effusions. By constraining air contamination in gases from Iceland, Eifel (Germany) and Yellowstone (USA), we derive estimates of mantle delta N-15 (the fractional difference in N-15/N-14 from air), N-2/Ar-36 and N-2/He-3. Our results show that negative delta N-15 values observed in gases, previously regarded as indicating a mantle origin for nitrogen(7-10), in fact represent dominantly air-derived N-2 that experienced N-15/N-14 fractionation in hydrothermal systems. Using two-component mixing models to correct for this effect, the (NN)-N-15-N-15 data allow extrapolations that characterize mantle endmember delta N-15, N-2/Ar-36 and N-2/He-3 values. We show that the Eifel region has slightly increased delta N-15 and N-2/Ar-36 values relative to estimates for the convective mantle provided by mid-ocean-ridge basalts(11), consistent with subducted nitrogen being added to the mantle source. In contrast, we find that whereas the Yellowstone plume has delta N-15 values substantially greater than that of the convective mantle, resembling surface components(12-15), its N-2/Ar-36 and N-2/He-3 ratios are indistinguishable from those of the convective mantle. This observation raises the possibility that the plume hosts a primordial component. We provide a test of the subduction hypothesis with a two-box model, describing the evolution of mantle and surface nitrogen through geological time. We show that the effect of subduction on the deep nitrogen cycle may be less important than has been suggested by previous investigations. We propose instead that high mid-ocean-ridge basalt and plume delta N-15 values may both be dominantly primordial features.


  
Laboratory Experiments of Volcanic Ash Resuspension by Wind 期刊论文
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2019, 124 (16) : 9534-9560
作者:  Etyemezian, V.;  Gillies, J. A.;  Mastin, L. G.;  Crawford, A.;  Hasson, R.;  Van Eaton, A. R.;  Nikolich, G.
收藏  |  浏览/下载:18/0  |  提交时间:2019/11/27
Mars  saltation  silica  basalt  volcano  aerosol  
Melting at the Edge of a Slab in the Deepest Mantle 期刊论文
GEOPHYSICAL RESEARCH LETTERS, 2019, 46 (14) : 8000-8008
作者:  Thorne, Michael S.;  Takeuchi, Nozomu;  Shiomi, Katsuhiko
收藏  |  浏览/下载:11/0  |  提交时间:2019/11/27
ultralow-velocity zone  mid-ocean ridge basalt  subduction  core-mantle boundary  
Volumetric and Shear Strain Localization in Mt. Etna Basalt 期刊论文
GEOPHYSICAL RESEARCH LETTERS, 2019, 46 (5) : 2425-2433
作者:  McBeck, Jessica A.;  Cordonnier, Benoit;  Vinciguerra, Sergio;  Renard, Francois
收藏  |  浏览/下载:12/0  |  提交时间:2019/11/26
strain localisation  digital volume correlation  basalt  X-ray microtomography  precursor  triaxial compression  
Noble gas signatures in the Island of Maui, Hawaii: Characterizing groundwater sources in fractured systems 期刊论文
WATER RESOURCES RESEARCH, 2017, 53 (5)
作者:  Niu, Yi;  Castro, M. Clara;  Hall, Chris M.;  Gingerich, Stephen B.;  Scholl, Martha A.;  Warrier, Rohit B.
收藏  |  浏览/下载:29/0  |  提交时间:2019/04/09
Maui Hawaii  noble gases  noble gas temperatures  basal aquifer  springs  mid-ocean ridge basalt