
Citation: | WU Jie, GAN Bo, SONG Wenhao, TANG Canlian, ZHANG Youjun. Shock-Induced Desulfurization of Natural Pyrite and Its Implications for the Early Earth’s Environment[J]. Chinese Journal of High Pressure Physics, 2025, 39(3): 030101. doi: 10.11858/gywlxb.20240916 |
泡沫金属质轻,具有较高的比刚度和比强度,以及隔热、电磁屏蔽等物理性能[1],在汽车交通、铁路、航空航天等领域广泛应用,如用于飞机外壳夹层、汽车防冲档。除此之外,泡沫金属在受到压缩时,由于其应变滞后于应力,压缩应力-应变曲线中有一个很长的低应力平台,可承受较大的塑性变形,因此泡沫金属具有良好的吸能特性,可用于缓和冲击的工程构件、能量吸收和防振构件[2]。
目前,常温下泡沫金属的静/动态本构关系已经得到广泛的研究。Chen和Lu[3]提出了一个依赖于特征应力和总应变的应力势,在此基础上建立了一个唯象的可压缩弹塑性本构模型的框架。该模型避免了人为区分应力-应变的弹塑性区带来的影响。王二恒等[4]利用Chen和Lu[3]提出的唯象本构模型框架,建立了一个泡沫金属准静态本构模型,得到了泡沫金属在三维等比例压缩和侧向受约束轴向压缩时的宏观应力-应变曲线。王志华等[5]提出了一个多参数的非线性弹塑性唯象本构模型,可以全面地描述泡沫金属材料线弹性段、应力平台段和密实段的典型三阶段变形特征。
泡沫金属是一种典型的低成本轻质材料,其复合结构有望作为近空间飞行器中的重要结构部件。但是,近空间飞行器苛刻的应用环境不但要求其结构轻质化,而且要求泡沫金属在高温下有较好的承载、隔热和冲击吸能能力。目前,考虑温度效应的泡沫金属力学行为的研究还比较少。Hakamada等[6]开展了ALPORAS闭孔泡沫铝及其基体材料在温度范围573~ 773 K内的准静态压缩试验,发现闭孔泡沫铝在高温下的变形机制与其基体材料的变形机制本质上是相同的。Aly[7]开展了ALPORAS闭孔泡沫铝在常温和高温下的压缩实验,研究了相对密度和实验温度的影响,研究发现,胞壁屈曲是闭孔泡沫铝的主要变形机制,增大密度与升高实验温度对泡沫金属力学性能的影响刚好相反。Cady等[8]研究了ALPORAS泡沫铝在不同应变率(0.001~1 800 s-1)和不同温度条件(77~295 K)下的力学性能,结果表明,闭孔泡沫铝的力学性能对温度具有很强的依赖性。
考虑泡沫金属温度效应的本构关系相关研究也比较匮乏。习会峰等[9]开展了-50~300 ℃范围内不同温度下泡沫铝的静态压缩实验,建立了考虑温度效应的泡沫铝静态压缩本构模型。王鹏飞等[10]基于Sherwood和Frost提出的本构关系框架,分析了泡沫铝本构方程中温度效应与应变率效应的耦合关系,对本构方程中的应变率敏感系数进行了适当修正,修正后的本构关系与实验结果的重合性较好,在此基础上得到了泡沫铝在一定密度范围内包含温度、应变率影响的较为完备的本构方程。
本研究通过开展不同密度(0.322~0.726 g/cm3)的泡沫铝在不同温度(25~500 ℃)下的准静态压缩实验,分析泡沫铝在不同温度下的力学性能,测得不同温度下泡沫铝的单轴压缩应力-应变曲线。基于Liu-Subhash模型[11],对不同温度下的实验数据进行拟合,建立考虑温度效应和密度效应的泡沫铝准静态压缩本构模型。
实验材料为闭孔泡沫铝,由上海奥深特金属复合材料科技有限公司提供。本研究采用的闭孔泡沫铝材料原尺寸为400 mm×400 mm×600 mm,孔径介于2~5 mm之间。准静态压缩实验采用线切割技术加工圆柱形试件。为了保证均匀性,排除胞孔尺寸影响,试件高度和直径不小于5个胞孔,试件尺寸为Ø32 mm×15 mm。实验前,对每个试样进行称量,得到其真实的相对密度,测得试样密度范围为0.322~0.796 g/cm3。
准静态实验在MTS810材料试验机上进行,加载速率为0.001 s-1。实验温度分别取25、200、275、350、425和500 ℃,高温实验在MTS810自带的高温箱中进行,温度误差为±5 ℃。
为了准确描述泡沫材料应力-应变曲线的三阶段特征,Liu与Subhash[11]提出了一维六参数本构模型
σ=p1ep2ε−1p6+ep3ε+ep4(ep5ε−1) |
(1) |
式中:σ为压缩应力,ε为压缩应变,p1、p2、p3、p4、p5和p6为用于描述泡沫材料性质的参数。p1主要描述压缩时屈服应力的变化;p2和p3为无量纲参数,主要描述应力平台阶段的硬化性能;p4和p5主要描述密实阶段的起点和密实阶段斜率的大小;p6主要描述弹性段斜率的大小。从模型中可以看出,参数p6的作用可以用p1和p3代替。习会峰等[9]提出简化模型,用常数1取代参数p6,将其简化为五参数模型
σ=p1ep2ε−11+ep3ε+ep4(ep5ε−1) |
(2) |
图 1为不同密度ρ下泡沫铝的准静态压缩应力-应变实验曲线。从实验结果来看,泡沫铝的应力-应变曲线的形状及发展趋势相似,呈典型的三阶段特性,即:较小应变下的线弹性阶段、对应于胞壁塑性坍塌而缓缓上升的应力平台阶段和密实后的应力迅速上升阶段。从图 1中可以看出,泡沫铝材料的初始密度对其应力-应变曲线影响巨大,随着密度的增大,曲线依次抬高,屈服强度也相应增大,但压缩至致密段的最大应变量减小。因此,在基体材料相同的情况下,在一定的密度范围内,泡沫铝材料的力学性能主要由材料的初始密度决定,初始密度越大,材料承载能力越强。
基于简化的Liu-Subhash模型,对实验得到的常温下不同密度泡沫铝的准静态应力-应变曲线进行拟合,得到不同密度泡沫铝材料的模型参数值,如表 1所示。实验曲线和拟合曲线如图 2所示,可见拟合效果较好,可采用该模型描述泡沫铝的单轴准静态压缩应力-应变关系。
Density/(g·cm-3) | Parameter | ||||
p1 | p2 | p3 | p4 | p5 | |
0.322 | 3.08 | 86.09 | 86.22 | -6.49 | 11.60 |
0.481 | 5.98 | 90.83 | 90.74 | -4.66 | 10.98 |
0.639 | 9.31 | 91.20 | 90.89 | -3.00 | 9.41 |
0.726 | 12.01 | 92.04 | 92.14 | -1.33 | 7.41 |
由表 1可知,参数p1、p2、p3、p4、p5随密度的变化而变化,显然这5个参数都是密度ρ的函数。因此,(2)式可以写成
σ=p1(ρ)ep2(ρ)ε−11+ep3(ρ)ε+ep4(ρ)[ep5(ρ)ε−1] |
(3) |
(3) 式即为考虑了密度影响的泡沫铝的常温准静态压缩本构模型。图 3为模型中5个参数随密度的变化情况,对实验数据进行拟合,得到5个参数与密度的关系为
{p1(ρ)=20.34ρ1.69p2(ρ)=94.58ρ0.08p3(ρ)=94.41ρ0.08p4(ρ)=12.34ρ−10.55p5(ρ)=−8.6ρ+14.68 |
(4) |
由(3)式和(4)式得到考虑密度效应的闭孔泡沫铝静态压缩本构模型,该模型可用于描述不同密度下泡沫铝的应力-应变曲线,具体形式如下
σ=20.34ρ1.69e94.58ρ0.08ε−11+e94.41ρ0.08ε+e12.34ρ−10.55[e(−8.6ρ+14.68)ε−1] |
(5) |
图 4是密度为0.322 g/cm3的泡沫铝在不同温度下的准静态应力-应变曲线。由图 4可知,随着温度的升高,材料由硬变软,由脆变韧。材料呈现明显的温度软化效应,当温度从25 ℃上升到500 ℃时,泡沫铝屈服强度从4.70 MPa下降到0.88 MPa。
为了得到包含温度效应的泡沫铝本构模型,引入温度软化项
H(T)=1−T∗m |
(6) |
式中:T*为无量纲温度项,m为指数。
T∗=T−TroomTmelt−Troom |
(7) |
式中:Troom为室温,Troom=298 K;Tmelt为铝合金的熔点,Tmelt=933 K。
因此,(3)式可进一步写成
σ={p1(ρ)ep2(ρ)ε−11+ep3(ρ)ε+ep4(ρ)[ep5(ρ)ε−1]}⋅[1−(T−TroomTmelt−Troom)m] |
(8) |
(8) 式即为考虑温度效应和密度效应的泡沫铝准静态本构模型。基于该模型,对不同温度下得到的准静态压缩应力-应变曲线进行拟合,得到参数m=1.31。不同温度下泡沫铝的应力-应变实验及拟合曲线如图 5所示。从图 5中可以看到,应力平台阶段和压实段拟合曲线与实验曲线吻合较好,说明该模型可用于描述不同温度下泡沫铝的应力-应变曲线。但在弹性段,拟合曲线与实验结果吻合得不太好,主要原因是Liu-Subhash模型不能很好地描述应力-应变曲线中的应力降现象,另一方面是由于实验时温度控制不精确产生的误差。总体上拟合曲线可以反映实验曲线的特征,拟合得到的参数值是可信的。
利用MTS万能材料试验机研究了不同密度(0.322~0.726 g/cm3)的闭孔泡沫铝在不同温度(25~500 ℃)下的静态压缩力学性能,实验结果表明:泡沫铝材料的初始密度对其应力-应变曲线影响巨大,随着密度的增大,屈服强度也相应增大,材料承载能力增强;随着温度的升高,泡沫铝材料力学特性由硬变软,呈现明显的温度软化效应。利用Liu-Subhash模型对不同密度下的实验数据进行拟合,拟合效果很好,分析并确定了模型中5个参数随密度变化的函数,并代入Liu-Subhash模型,得到了考虑密度效应的本构模型;又引入温度软化项对本构模型进行修正,建立了综合考虑温度效应和密度效应的泡沫铝准静态压缩本构模型。
[1] |
GRIEVE R A F. The record of impact on Earth: implications for a major Cretaceous/Tertiary impact event [M]//SILVER L T, SCHULTZ P H. Geological Implications of Impacts of Large Asteroids and Comets on the Earth. Boulder: Geological Society of America, 1982: 25−38.
|
[2] |
RAUP D M. Biological extinction in earth history [J]. Science, 1986, 231(4745): 1528–1533. doi: 10.1126/science.11542058
|
[3] |
JUNIUM C K, ZERKLE A L, WITTS J D, et al. Massive perturbations to atmospheric sulfur in the aftermath of the Chicxulub impact [J]. Proceedings of the National Academy of Sciences of the United States of America, 2022, 119(14): e2119194119. doi: 10.1073/pnas.2119194119
|
[4] |
SCHMIEDER M, KRING D A. Earth’s impact events through geologic time: a list of recommended ages for terrestrial impact structures and deposits [J]. Astrobiology, 2020, 20(1): 91–141. doi: 10.1089/ast.2019.2085
|
[5] |
GAY N C. Spherules on shatter cone surfaces from the vredefort structure, South Africa [J]. Science, 1976, 194(4266): 724–725. doi: 10.1126/science.194.4266.724
|
[6] |
ALLEN N H, NAKAJIMA M, WÜNNEMANN K, et al. A revision of the formation conditions of the vredefort crater [J]. Journal of Geophysical Research: Planets, 2022, 127(8): e2022JE007186. doi: 10.1029/2022JE007186
|
[7] |
ALVAREZ W, CLAEYS P, KIEFFER S W. Emplacement of cretaceous-tertiary boundary shocked quartz from Chicxulub crater [J]. Science, 1995, 269(5226): 930–935. doi: 10.1126/science.269.5226.930
|
[8] |
SCHULTE P, ALEGRET L, ARENILLAS I, et al. The Chicxulub asteroid impact and mass extinction at the cretaceous-paleogene boundary [J]. Science, 2010, 327(5970): 1214–1218. doi: 10.1126/science.1177265
|
[9] |
POPE K O, BAINES K H, OCAMPO A C, et al. Energy, volatile production, and climatic effects of the Chicxulub Cretaceous/Tertiary impact [J]. Journal of Geophysical Research: Planets, 1997, 102(E9): 21645–21664. doi: 10.1029/97JE01743
|
[10] |
KAWARAGI K, SEKINE Y, KADONO T, et al. Direct measurements of chemical composition of shock-induced gases from calcite: an intense global warming after the Chicxulub impact due to the indirect greenhouse effect of carbon monoxide [J]. Earth and Planetary Science Letters, 2009, 282(1/2/3/4): 56–64. doi: 10.1016/j.jpgl.2009.02.037
|
[11] |
VON GEHLEN K. Sulfur in the Earth’s mantle—a review [M]//SCHIDLOWSKI M, GOLUBIC S, KIMBERLEY M M, et al. Early Organic Evolution. Berlin: Springer, 1992: 359−366.
|
[12] |
WALTERS J B, CRUZ-URIBE A M, MARSCHALL H R. Sulfur loss from subducted altered oceanic crust and implications for mantle oxidation [J]. Geochemical Perspectives Letters, 2020, 13: 36–41. doi: 10.7185/geochemlet.2011
|
[13] |
CHOWDHURY P, DASGUPTA R. Sulfur extraction via carbonated melts from sulfide-bearing mantle lithologies-implications for deep sulfur cycle and mantle redox [J]. Geochimica et Cosmochimica Acta, 2020, 269: 376–397. doi: 10.1016/j.gca.2019.11.002
|
[14] |
PIERAZZO E, HAHMANN A N, SLOAN L C. Chicxulub and climate: radiative perturbations of impact-produced S-bearing gases [J]. Astrobiology, 2003, 3(1): 99–118. doi: 10.1089/153110703321632453
|
[15] |
MORGAN J V, BRALOWER T J, BRUGGER J, et al. The Chicxulub impact and its environmental consequences [J]. Nature Reviews Earth & Environment, 2022, 3(5): 338–354. doi: 10.1038/s43017-022-00283-y
|
[16] |
KAIHO K, KAJIWARA Y, NAKANO T, et al. End-Permian catastrophe by a bolide impact: evidence of a gigantic release of sulfur from the mantle [J]. Geology, 2001, 29(9): 815–818. doi: 10.1130/0091-7613(2001)029<0815:EPCBAB>2.0.CO;2
|
[17] |
BRENNECKA G A, HERRMANN A D, ALGEO T J, et al. Rapid expansion of oceanic anoxia immediately before the end-Permian mass extinction [J]. Proceedings of the National Academy of Sciences of the United States of America, 2011, 108(43): 17631–17634. doi: 10.1073/pnas.1106039108
|
[18] |
ZHANG H, ZHANG F F, CHEN J B, et al. Felsic volcanism as a factor driving the end-Permian mass extinction [J]. Science Advances, 2021, 7(47): eabh1390. doi: 10.1126/sciadv.abh1390
|
[19] |
BECKER L, POREDA R J, BASU A R, et al. Bedout: a possible end-Permian impact crater offshore of Northwestern Australia [J]. Science, 2004, 304(5676): 1469–1476. doi: 10.1126/science.1093925
|
[20] |
JIANG Y F, TANG Y G, CHOU C L. Research on genesis of pyrite near the Permian-Triassic boundary in Meishan, Zhejiang, China [J]. Journal of China University of Mining and Technology, 2006, 16(4): 457–460. doi: 10.1016/S1006-1266(07)60047-9
|
[21] |
SALISBURY J, GRÖCKE D R, CHEUNG H D R A, et al. An 80-million-year sulphur isotope record of pyrite burial over the Permian-Triassic [J]. Scientific Reports, 2022, 12(1): 17370. doi: 10.1038/s41598-022-21542-4
|
[22] |
SHEN W J, LIN Y T, XU L, et al. Pyrite framboids in the Permian-Triassic boundary section at Meishan, China: evidence for dysoxic deposition [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2007, 253(3/4): 323–331. doi: 10.1016/j.palaeo.2007.06.005
|
[23] |
AHMED M A, ELLID M S, AMAMI S, et al. Mössbauer study of the thermal decomposition of pyrite in one Egyptian coal heated in hydrogen atmosphere at different temperatures (438 K–715 K) [J]. Arabian Journal for Science and Engineering, 2006, 31(2A): 159–165.
|
[24] |
HU G L, DAM-JOHANSEN K, WEDEL S, et al. Decomposition and oxidation of pyrite [J]. Progress in Energy and Combustion Science, 2006, 32(3): 295–314. doi: 10.1016/j.pecs.2005.11.004
|
[25] |
XU H W, GUO X F, SEAMAN L A, et al. Thermal desulfurization of pyrite: an in situ high-T neutron diffraction and DTA-TGA study [J]. Journal of Materials Research, 2019, 34(19): 3243–3253. doi: 10.1557/jmr.2019.185
|
[26] |
SHARP W E. Melting curves of sphalerite, galena, and pyrrhotite and the decomposition curve of pyrite between 30 and 65 kilobars [J]. Journal of Geophysical Research, 1969, 74(6): 1645–1652. doi: 10.1029/JB074i006p01645
|
[27] |
ZHMODIK S M, VERKHOVTSEVA N V, CHIKOV B M, et al. Experimental study of gold redistribution in a shock-metamorphosed pyrite-quartz mixture with the use of the 195Au radionuclide [J]. Geochemistry International, 2004, 42(12): 1139–1153.
|
[28] |
MOROSIN B, GRAHAM R A, POLLACK S S. X-ray diffraction line broadening in shock modified pyrite [M]//SCHMIDT S C, DICK R D, FORBES J W, et al. Shock Compression of Condensed Matter–1991. Amsterdam: North-Holland, 1992: 613−616.
|
[29] |
POLLACK S S, MARTELLO D V, GRAHAM R A, et al. Reactivity of pyrites and dislocation density [M]//International Energy Agency Coal Research Ltd. 1991 International Conference on Coal Science Proceedings. Butterworth-Heinemann, 1991: 885−888.
|
[30] |
SCLAR C B, USSELMAN T M. Experimentally induced shock effects in some rock-forming minerals [J]. Meteoritics, 1970, 5: 222–223.
|
[31] |
AHRENS T J. Equations of state of iron sulfide and constraints on the sulfur content of the Earth [J]. Journal of Geophysical Research: Solid Earth, 1979, 84(B3): 985–998. doi: 10.1029/JB084iB03p00985
|
[32] |
AHRENS T J, JEANLOZ R. Pyrite: shock compression, isentropic release, and composition of the Earth’s core [J]. Journal of Geophysical Research: Solid Earth, 1987, 92(B10): 10363–10375. doi: 10.1029/JB092iB10p10363
|
[33] |
ANDERSON W W, AHRENS T J. Shock temperature and melting in iron sulfides at core pressures [J]. Journal of Geophysical Research: Solid Earth, 1996, 101(B3): 5627–5642. doi: 10.1029/95JB01972
|
[34] |
LANGENHORST F, BOUSTIE M, DEUTSCH A, et al. Experimental techniques for the simulation of shock metamorphism: a case study on calcite [M]//DAVISON L, HORIE Y, SEKINE T. High-Pressure Shock Compression of Solids V. New York: Springer, 2003: 1−27.
|
[35] |
MARTINEZ I, DEUTSCH A, SCHÄRER U, et al. Shock recovery experiments on dolomite and thermodynamical calculations of impact induced decarbonation [J]. Journal of Geophysical Research: Solid Earth, 1995, 100(B8): 15465–15476. doi: 10.1029/95JB01151
|
[36] |
MANSFELD U, LANGENHORST F, EBERT M, et al. Microscopic evidence of stishovite generated in low-pressure shock experiments on porous sandstone: constraints on its genesis [J]. Meteoritics & Planetary Science, 2017, 52(7): 1449–1464. doi: 10.1111/maps.12867
|
[37] |
ZHANG F P, SEKINE T. Impact-shock behavior of Mg- and Ca-sulfates and their hydrates [J]. Geochimica et Cosmochimica Acta, 2007, 71(16): 4125–4133. doi: 10.1016/j.gca.2007.06.037
|
[38] |
KUROSAWA K, MORIWAKI R, KOMATSU G, et al. Shock vaporization/devolatilization of evaporitic minerals, halite and gypsum, in an open system investigated by a two-stage light gas gun [J]. Geophysical Research Letters, 2019, 46(13): 7258–7267. doi: 10.1029/2019GL083249
|
[39] |
PRESCHER C, LANGENHORST F, HORNEMANN U, et al. Shock experiments on anhydrite and new constraints on the impact-induced SO x release at the K-Pg boundary [J]. Meteoritics & Planetary Science, 2011, 46(11): 1619–1629. doi: 10.1111/j.1945-5100.2011.01249.x
|
[40] |
GRIEVE R A F, LANGENHORST F, STÖFFLER D. Shock metamorphism of quartz in nature and experiment: Ⅱ. significance in geoscience [J]. Meteoritics & Planetary Science, 1996, 31(1): 6–35. doi: 10.1111/j.1945-5100.1996.tb02049.x
|
[41] |
THOMPSON E C, CHIDESTER B A, FISCHER R A, et al. Equation of state of pyrite to 80 GPa and 2400 K [J]. American Mineralogist, 2016, 101(5): 1046–1051. doi: 10.2138/am-2016-5527
|
[42] |
ZHANG Y J, SEKINE T, LIN J F, et al. Shock compression and melting of an Fe-Ni-Si alloy: implications for the temperature profile of the Earth’s core and the heat flux across the core-mantle boundary [J]. Journal of Geophysical Research: Solid Earth, 2018, 123(2): 1314–1327. doi: 10.1002/2017JB014723
|
[43] |
KRAUS R G, DAVIS J P, SEAGLE C T, et al. Dynamic compression of copper to over 450 GPa: a high-pressure standard [J]. Physical Review B, 2016, 93(13): 134105. doi: 10.1103/PhysRevB.93.134105
|
[44] |
DAI C D, HU J B, TAN H. Hugoniot temperatures and melting of tantalum under shock compression determined by optical pyrometry [J]. Journal of Applied Physics, 2009, 106(4): 043519. doi: 10.1063/1.3204941
|
[45] |
MITCHELL A C, NELLIS W J. Shock compression of aluminum, copper, and tantalum [J]. Journal of Applied Physics, 1981, 52(5): 3363–3374. doi: 10.1063/1.329160
|
[46] |
SEILER F, IGRA O. Hypervelocity launchers [M]. Cham: Springer, 2016.
|
[47] |
WANG H P, SALVESON I. A review on the mineral chemistry of the non-stoichiometric iron sulphide, Fe1− xS (0≤x≤0.125): polymorphs, phase relations and transitions, electronic and magnetic structures [J]. Phase Transitions, 2005, 78(7/8): 547–567. doi: 10.1080/01411590500185542
|
[48] |
GAN B, ZHANG Y J, HUANG Y Q, et al. Partial deoxygenation and dehydration of ferric oxyhydroxide in Earth’s subducting slabs [J]. Geophysical Research Letters, 2021, 48(17): e2021GL094446. doi: 10.1029/2021GL094446
|
[49] |
MANG C, KONTNY A, FRITZ J, et al. Shock experiments up to 30 GPa and their consequences on microstructures and magnetic properties in pyrrhotite [J]. Geochemistry, Geophysics, Geosystems, 2013, 14(1): 64–85. doi: 10.1029/2012GC004242
|
[50] |
LEROUX H, REIMOLD W U, KOEBERL C, et al. Experimental shock deformation in zircon: a transmission electron microscopic study [J]. Earth and Planetary Science Letters, 1999, 169(3/4): 291–301. doi: 10.1016/S0012-821X(99)00082-5
|
[51] |
RAO M N, NYQUIST L E, ASIMOW P D, et al. Shock experiments on basalt-ferric sulfate mixes and their possible relevance to the sulfide bleb clusters in large impact melts in shergottites [J]. Meteoritics & Planetary Science, 2021, 56(12): 2250–2264. doi: 10.1111/maps.13770
|
[52] |
RAO M N, NYQUIST L E, ROSS D K, et al. Signatures of the Martian regolith components entrained in some impact-melt glasses in shergottites [J]. Meteoritics & Planetary Science, 2018, 53(12): 2558–2582. doi: 10.1111/maps.13177
|
[53] |
DENG J S, WEN S M, CHEN X M, et al. Dynamic simulation of the thermal decomposition of pyrite under vacuum [J]. Metallurgical and Materials Transactions A, 2014, 45(5): 2445–2452. doi: 10.1007/s11661-014-2206-4
|
[54] |
LANGE M A, LAMBERT P, AHRENS T J. Shock effects on hydrous minerals and implications for carbonaceous meteorites [J]. Geochimica et Cosmochimica Acta, 1985, 49(8): 1715–1726. doi: 10.1016/0016-7037(85)90142-5
|
[55] |
MEYERS M A, ANDRADE U R, CHOKSHI A H. The effect of grain size on the high-strain, high-strain-rate behavior of copper [J]. Metallurgical and Materials Transactions A, 1995, 26(11): 2881–2893. doi: 10.1007/BF02669646
|
[56] |
SCHMITT R T. Shock experiments with the H6 chondrite Kernouvé: pressure calibration of microscopic shock effects [J]. Meteoritics & Planetary Science, 2000, 35(3): 545–560. doi: 10.1111/j.1945-5100.2000.tb01435.x
|
[57] |
苏林祥. 《实验物态方程导引》简介 [J]. 爆炸与冲击, 1987, 7(1): 84. doi: 10.11883/1001-1455(1987)01-0084-1
SU L X. Introduction to the “equation of state for experimental states” [J]. Explosion and Shock Waves, 1987, 7(1): 84. doi: 10.11883/1001-1455(1987)01-0084-1
|
[58] |
GRAY Ⅲ G T. Shock recovery experiments: an assessment [C]//American Physical Society Topical Conference on Shock Compression of Condensed Matter. Albuquerque, 1989.
|
[59] |
WILLIAMS C L, ZIMMERMAN K B. Structure-property relationships under extreme dynamic environments: shock recovery experiments [M]. Cham: Springer, 2019.
|
[60] |
SEKINE T. Shock-induced chemistry [M]. Singapore: Springer, 2024.
|
[61] |
RAIKES S A, AHRENS T J. Post-shock temperatures in minerals [J]. Geophysical Journal International, 1979, 58(3): 717–747. doi: 10.1111/j.1365-246X.1979.tb04804.x
|
[62] |
GRAY Ⅲ G T, FOLLANSBEE P S, FRANTZ C E. Effect of residual strain on the substructure development and mechanical response of shock-loaded copper [J]. Materials Science and Engineering: A, 1989, 111: 9–16. doi: 10.1016/0921-5093(89)90192-5
|
[63] |
GRAY Ⅲ G T. Influence of shock-wave deformation on the structure/property behavior of materials [M]//ASAY J R, SHAHINPOOR M. High-Pressure Shock Compression of Solids. New York: Springer, 1993: 187−215.
|
[64] |
HU J P, ASIMOW P D, MA C, et al. First synthesis of a unique icosahedral phase from the Khatyrka meteorite by shock-recovery experiment [J]. IUCrJ, 2020, 7(3): 434–444. doi: 10.1107/S2052252520002729
|
[65] |
BECKER L, POREDA R J, HUNT A G, et al. Impact event at the Permian-Triassic boundary: evidence from extraterrestrial noble gases in fullerenes [J]. Science, 2001, 291(5508): 1530–1533. doi: 10.1126/science.1057243
|
[66] |
BELL M S. CO2 release due to impact devolatilization of carbonate: results of shock experiments [J]. Meteoritics & Planetary Science, 2016, 51(4): 619–646. doi: 10.1111/maps.12613
|
[67] |
FRITZ J, GRESHAKE A, FERNANDES V A. Revising the shock classification of meteorites [J]. Meteoritics & Planetary Science, 2017, 52(6): 1216–1232. doi: 10.1111/maps.12845
|
[68] |
STÖFFLER D, KEIL K, SCOTT E R D. Shock metamorphism of ordinary chondrites [J]. Geochimica et Cosmochimica Acta, 1991, 55(12): 3845–3867. doi: 10.1016/0016-7037(91)90078-J
|
[69] |
RUBIN A E. Smyer H-chondrite impact-melt breccia and evidence for sulfur vaporization [J]. Geochimica et Cosmochimica Acta, 2002, 66(4): 699–711. doi: 10.1016/S0016-7037(01)00799-2
|
[70] |
BENNETT III M E, MCSWEEN H Y. Shock features in iron-nickel metal and troilite of L-group ordinary chondrites [J]. Meteoritics & Planetary Science, 1996, 31(2): 255–264. doi: 10.1111/j.1945-5100.1996.tb02021.x
|
[71] |
DAI C D, JIN X G, FU S Q, et al. The equation-of-states of Jilin ordinary chondrite and Nandan iron meteorite [J]. Science in China Series D: Earth Sciences, 1997, 40(4): 403–410. doi: 10.1007/BF02877572
|
[72] |
STÖFFLER D, BISCHOFF A, BUCHWALD V, et al. Shock effects in meteorites [M]. Meteorites and the Early Solar System, 1988.
|
[73] |
HU J P, SHARP T G. Formation, preservation and extinction of high-pressure minerals in meteorites: temperature effects in shock metamorphism and shock classification [J]. Progress in Earth and Planetary Science, 2022, 9(1): 6. doi: 10.1186/s40645-021-00463-2
|
[74] |
IVANOV B A. Mars/moon cratering rate ratio estimates [J]. Space Science Reviews, 2001, 96(1/2/3/4): 87–104. doi: 10.1023/A:1011941121102
|
[75] |
FARINELLA P, DAVIS D R. Collision rates and impact velocities in the main asteroid belt [J]. Icarus, 1992, 97(1): 111–123. doi: 10.1016/0019-1035(92)90060-K
|
[76] |
SAITO T, KAIHO K, ABE A, et al. Hypervelocity impact of asteroid/comet on the oceanic crust of the Earth [J]. International Journal of Impact Engineering, 2008, 35(12): 1770–1777. doi: 10.1016/j.ijimpeng.2008.07.046
|
[77] |
SAITO T, KAIHO K, ABE A, et al. Numerical simulations of hypervelocity impact of asteroid/comet on the Earth [J]. International Journal of Impact Engineering, 2006, 33(1): 713−722.
|
[78] |
LI M H, FRANK T D, XU Y L, et al. Sulfur isotopes link atmospheric sulfate aerosols from the Siberian Traps outgassing to the end-Permian extinction on land [J]. Earth and Planetary Science Letters, 2022, 592: 117634. doi: 10.1016/j.jpgl.2022.117634
|
[79] |
KAIHO K, KAJIWARA Y, CHEN Z Q, et al. A sulfur isotope event at the end of the Permian [J]. Chemical Geology, 2006, 235(1/2): 33–47. doi: 10.1016/j.chemgeo.2006.06.001
|
[80] |
ERWIN D H, BOWRING S A, YUGAN J. End-Permian mass extinctions: a review [M]//KOEBERL C, MACLEOD K G. Catastrophic Events and Mass Extinctions: Impacts and Beyond. Boulder: Geological Society of America, 2002.
|
[81] |
RUBIN A E. Maskelynite in asteroidal, lunar and planetary basaltic meteorites: an indicator of shock pressure during impact ejection from their parent bodies [J]. Icarus, 2015, 257: 221–229. doi: 10.1016/j.icarus.2015.05.010
|
[82] |
GENG S J, ZHOU B H, LI M T. On the capture of small stony asteroids into the Earth’s orbit by atmospheric grazing [J]. Monthly Notices of the Royal Astronomical Society, 2021, 507(3): 4661–4668. doi: 10.1093/mnras/stab2439
|
[83] |
MAHOWALD N, WARD D S, KLOSTER S, et al. Aerosol impacts on climate and biogeochemistry [J]. Annual Review of Environment and Resources, 2011, 36: 45–74. doi: 10.1146/annurev-environ-042009-094507
|
[84] |
FINLAYSON-PITTS B J, PITTS J N JR. Chemistry of the upper and lower atmosphere [M]. San Diego: Academic Press, 2000.
|
[85] |
MACDONALD F A, WORDSWORTH R. Initiation of Snowball Earth with volcanic sulfur aerosol emissions [J]. Geophysical Research Letters, 2017, 44(4): 1938–1946. doi: 10.1002/2016GL072335
|
[86] |
STERN R J, AVIGAD D, MILLER N, et al. From volcanic winter to snowball Earth: an alternative explanation for neoproterozoic biosphere stress [M]//DILEK Y, FURNES H, MUEHLENBACHS K. Links Between Geological Processes, Microbial Activities & Evolution of Life: Microbes and Geology. Dordrecht: Springer, 2008: 313−337.
|
[87] |
FAN S M, JACOB D J. Surface ozone depletion in Arctic spring sustained by bromine reactions on aerosols [J]. Nature, 1992, 359(6395): 522–524. doi: 10.1038/359522a0
|
[88] |
PORTMANN R W, SOLOMON S, GARCIA R R, et al. Role of aerosol variations in anthropogenic ozone depletion in the polar regions [J]. Journal of Geophysical Research: Atmospheres, 1996, 101(D17): 22991–23006. doi: 10.1029/96JD02608
|
[89] |
TABAZADEH A, DRDLA K, SCHOEBERL M R, et al. Arctic “ozone hole” in a cold volcanic stratosphere [J]. Proceedings of the National Academy of Sciences of the United States of America, 2002, 99(5): 2609–2612. doi: 10.1073/pnas.052518199
|
[90] |
BENCA J P, DUIJNSTEE I A P, LOOY C V. UV-B-induced forest sterility: implications of ozone shield failure in Earth’s largest extinction [J]. Science Advances, 2018, 4(2): e1700618. doi: 10.1126/sciadv.1700618
|
[91] |
VISSCHER H, LOOY C V, COLLINSON M E, et al. Environmental mutagenesis during the end-Permian ecological crisis [J]. Proceedings of the National Academy of Sciences of the United States of America, 2004, 101(35): 12952–12956. doi: 10.1073/pnas.0404472101
|
[92] |
BLACK B A, LAMARQUE J F, SHIELDS C A, et al. Acid rain and ozone depletion from pulsed Siberian Traps magmatism [J]. Geology, 2014, 42(1): 67–70. doi: 10.1130/G34875.1
|
[93] |
LI R C, SHEN S Z, XIA X P, et al. Atmospheric ozone destruction and the end-Permian crisis: evidence from multiple sulfur isotopes [J]. Chemical Geology, 2024, 647: 121936. doi: 10.1016/j.chemgeo.2024.121936
|
[94] |
JURIKOVA H, GUTJAHR M, WALLMANN K, et al. Permian-Triassic mass extinction pulses driven by major marine carbon cycle perturbations [J]. Nature Geoscience, 2020, 13(11): 745–750. doi: 10.1038/s41561-020-00646-4
|
[1] | LIU Yushi, ZHANG Long, LI Wenguang, LIU Qijun, LIU Zhengtang, LIU Fusheng. First-Principles Investigation of the High-Pressure Phase Transition in Representative Alkali Metal Halides[J]. Chinese Journal of High Pressure Physics, 2025, 39(2): 022201. doi: 10.11858/gywlxb.20240864 |
[2] | MA Hao, CHEN Ling, JIANG Qiwen, AN Decheng, DUAN Defang. Ab Initio Calculation Principles Study of Crystal Structure and Superconducting Properties of Y-Si-H System under High Pressure[J]. Chinese Journal of High Pressure Physics, 2024, 38(2): 020106. doi: 10.11858/gywlxb.20230791 |
[3] | WANG Xiaoxue, DING Yuqing, WANG Hui. First-Principles Study of the High-Pressure Phase Transition and Physical Properties of Rubidium Nitrate[J]. Chinese Journal of High Pressure Physics, 2024, 38(4): 040103. doi: 10.11858/gywlxb.20240776 |
[4] | WANG Xiaoxue, DING Yuqing, WANG Hui. First-Principles Study of the Dynamics in Face-Centered Cubic CeH9 and CeH10 under High Pressure[J]. Chinese Journal of High Pressure Physics, 2024, 38(2): 020109. doi: 10.11858/gywlxb.20230771 |
[5] | ZHANG Chang, SUN Xiaowei, SONG Ting, TIAN Junhong, LIU Zijiang. First-Principles Study on Mechanical Properties of Sc, Ti, V, Zr-Doped Cr2B3 at High Pressure[J]. Chinese Journal of High Pressure Physics, 2022, 36(4): 042201. doi: 10.11858/gywlxb.20210916 |
[6] | XIE Yafei, JIANG Changguo, LUO Xingli, TAN Dayong, XIAO Wansheng. Synthesis of 6H-Type Hexagonal Perovskite Phase of BaGeO3 at High Temperature and High Pressure[J]. Chinese Journal of High Pressure Physics, 2021, 35(5): 051201. doi: 10.11858/gywlxb.20210761 |
[7] | WU Xiao, MA Yangyang, YANG Shu, HE Kaihua, JI Guangfu. First Principles Study of Lattice Thermal Conductivity and Sound Velocity Characteristics of FeO2 and FeO2He[J]. Chinese Journal of High Pressure Physics, 2021, 35(3): 032201. doi: 10.11858/gywlxb.20200659 |
[8] | WEN Xinzhu, PENG Yuyan, LIU Mingzhen. First-Principles Study on Structural Stability of Perovskite ZrBeO3[J]. Chinese Journal of High Pressure Physics, 2020, 34(1): 011202. doi: 10.11858/gywlxb.20190802 |
[9] | YANG Longxing, LIU Lei, LIU Hong, YI Li, GU Xiaoyu. Structure and Elasticity of Garnet under High Pressure by First-Principles Simulation[J]. Chinese Journal of High Pressure Physics, 2019, 33(6): 060104. doi: 10.11858/gywlxb.20190785 |
[10] | LIU Siyuan, MIAO Yu, MA Xuejiao, LI Xin, GAO Wenquan, CHENG Yuheng, LIU Yanhui. Pressure-Induced Phase Transformations of IrSb from First-Principles Calculations[J]. Chinese Journal of High Pressure Physics, 2019, 33(5): 052203. doi: 10.11858/gywlxb.20190716 |
[11] | ZHANG Leting, ZHAO Yuhong, SUN Yuanyang, DENG Shijie, JI Ruyi, HAN Peide. Thermodynamic Properties of Mg2X (X=Si, Ge) Phases under Pressure by First-Principles Calculations[J]. Chinese Journal of High Pressure Physics, 2018, 32(3): 032201. doi: 10.11858/gywlxb.20170630 |
[12] | HAN Lin, MA Mai-Ning, XU Zhi-Shuang, ZHOU Xiao-Ya. Structural Properties and Phase Transition of Pyroxene Polymorphs from First-Principles[J]. Chinese Journal of High Pressure Physics, 2017, 31(2): 125-134. doi: 10.11858/gywlxb.2017.02.004 |
[13] | REN Xiao-Guang, CUI Xue-Han, WU Bao-Jia, GU Guang-Rui. Electronic Structure and Lattice Dynamics of Intermetallic Compounds CaAlSi at High-Pressure[J]. Chinese Journal of High Pressure Physics, 2014, 28(2): 161-167. doi: 10.11858/gywlxb.2014.02.005 |
[14] | TAN Xin, JIA Yi-Chao, LIU Xue-Jie. First-Principles Investigations on Phase Transition of ZrN under External Pressure[J]. Chinese Journal of High Pressure Physics, 2014, 28(2): 168-174. doi: 10.11858/gywlxb.2014.02.006 |
[15] | DENG Li, LIU Hong, TIAN Hua, DU Jian-Guo, LIU Lei. First-Principles Molecular Dynamics Study of the Structure of MgSiO3 Melt at High Temperatures and High Pressures[J]. Chinese Journal of High Pressure Physics, 2014, 28(3): 273-282. doi: 10.11858/gywlxb.2014.03.003 |
[16] | DING Ying-Chun, LIU Hai-Jun, JIANG Meng-Heng, CHEN Min, CHEN Yong-Ming. First-Principles Investigations on Structural Transformation and Electronic Properties of BeP2N4 under High Pressure[J]. Chinese Journal of High Pressure Physics, 2012, 26(6): 674-680. doi: 10.11858/gywlxb.2012.06.012 |
[17] | HAO Jun-Hua, WU Zhi-Qiang, WANG Zheng, JIN Qing-Hua, LI Bao-Hui, DING Da-Tong. First Principles Calculation of SiO2 at High Pressures[J]. Chinese Journal of High Pressure Physics, 2010, 24(4): 260-266 . doi: 10.11858/gywlxb.2010.04.004 |
[18] | LIU Xiao-Yang, ZHAO Xu-Dong, HOU Wei-Min, SU Wen-Hui. Transformation of Boron Oxide B2O3 under High Pressure and High Temperature[J]. Chinese Journal of High Pressure Physics, 1995, 9(3): 213-217 . doi: 10.11858/gywlxb.1995.03.009 |
[19] | XIONG Da-He. Isothermal Compression and High Pressure Phase Transformation of Nickel Oxide (Bunsenite)[J]. Chinese Journal of High Pressure Physics, 1991, 5(3): 169-176 . doi: 10.11858/gywlxb.1991.03.002 |
[20] | WENG Ke-Nan. Lattice Parameters of the Perovskite in Aluminum-Bearing Silicates[J]. Chinese Journal of High Pressure Physics, 1987, 1(2): 102-109 . doi: 10.11858/gywlxb.1987.02.002 |
Density/(g·cm-3) | Parameter | ||||
p1 | p2 | p3 | p4 | p5 | |
0.322 | 3.08 | 86.09 | 86.22 | -6.49 | 11.60 |
0.481 | 5.98 | 90.83 | 90.74 | -4.66 | 10.98 |
0.639 | 9.31 | 91.20 | 90.89 | -3.00 | 9.41 |
0.726 | 12.01 | 92.04 | 92.14 | -1.33 | 7.41 |