We estimated crustal v p/ v s ratio of Tibetan Plateau by combined inversion of Love and Rayleigh wave dispersion data. It is developed by us that the joint inversion methods using both Love and Rayleigh wave dispersi...We estimated crustal v p/ v s ratio of Tibetan Plateau by combined inversion of Love and Rayleigh wave dispersion data. It is developed by us that the joint inversion methods using both Love and Rayleigh wave dispersion data. Thickness and S\|wave velocity of each sub layer are taken from Love wave dispersion data, then P\|wave velocity structure was deduced using Rayleigh wave dispersion data. Densities of sub layers were estimated by the empirical relationships between seismic velocity and rock density. Having S\| and P\|wave velocities, v p/ v s ratio is calculated for each sub layer. Six sub layers in crust of Tibetan Plateau has been identified, which are 0～8km, 8～30km, 30～40km, 40～62km, 62～68km and 68～75km respectively. The S\|wave velocity structure of the Plateau is 3 13, 3 32, 3 15, 3 92, 3 45 and 3 87 km/s for each sub layer; and P\|wave velocities are 6 00, 6 10, 5 72, 6 35, 6 78 and 6 64km/s respectively v p/ v s ratios in sub layers are 1 92, 1 84, 1 82, 1 62, 1 96 and 1 72; and corresponding Poisson ratios are 0 31, 0 29, 0 28, 0 19, 0 32 and 0 24. Our result on Poisson ratios of Tibetan crust was supported by seismic waveform modelling by Rodgers and Schwartz (1998).展开更多
以西北农林科技大学校园内生长良好的耐旱树种刺槐(R obin ia p seud oacacia L.)、元宝枫(A certrunca tum Bge.)、沙棘(H ipp ophae rham noid es L.)、白榆(U lm us pum ila L.)、油松(P inus tabu laef orm is C arr.)、白皮松(P in...以西北农林科技大学校园内生长良好的耐旱树种刺槐(R obin ia p seud oacacia L.)、元宝枫(A certrunca tum Bge.)、沙棘(H ipp ophae rham noid es L.)、白榆(U lm us pum ila L.)、油松(P inus tabu laef orm is C arr.)、白皮松(P inus bung eana Zucc.ex End l.)及中生树种女贞(L igustrum lucidum A it.)和柳树(S a lix m a tsud ana K o idz.f.p endu la Schne id)为研究对象,用压力套在2.5 M Pa下诱导1年生枝条发生木质部栓塞,研究自然条件下木质部栓塞的恢复特性,探讨木质部栓塞恢复特性与PV曲线水分参数间的关系。结果表明,木质部栓塞恢复的快慢,与其小枝的木质部栓塞脆弱性顺序基本一致;栓塞的发生和恢复与树木木质部的结构密切相关。植物木质部栓塞的发生、恢复,与植物耐旱性一样受多种因素控制,虽然与PV曲线水分参数有一定关系,但任何单一水分参数的排序,均与木质部栓塞的脆弱性和恢复速率不完全一致。木质部水势和树木不同部位间的水势梯度是影响木质部栓塞发生和恢复的最主要因素,蒸腾作用、气孔关闭及植物的渗透调节等可能也与木质部栓塞的恢复有关。展开更多
文摘We estimated crustal v p/ v s ratio of Tibetan Plateau by combined inversion of Love and Rayleigh wave dispersion data. It is developed by us that the joint inversion methods using both Love and Rayleigh wave dispersion data. Thickness and S\|wave velocity of each sub layer are taken from Love wave dispersion data, then P\|wave velocity structure was deduced using Rayleigh wave dispersion data. Densities of sub layers were estimated by the empirical relationships between seismic velocity and rock density. Having S\| and P\|wave velocities, v p/ v s ratio is calculated for each sub layer. Six sub layers in crust of Tibetan Plateau has been identified, which are 0～8km, 8～30km, 30～40km, 40～62km, 62～68km and 68～75km respectively. The S\|wave velocity structure of the Plateau is 3 13, 3 32, 3 15, 3 92, 3 45 and 3 87 km/s for each sub layer; and P\|wave velocities are 6 00, 6 10, 5 72, 6 35, 6 78 and 6 64km/s respectively v p/ v s ratios in sub layers are 1 92, 1 84, 1 82, 1 62, 1 96 and 1 72; and corresponding Poisson ratios are 0 31, 0 29, 0 28, 0 19, 0 32 and 0 24. Our result on Poisson ratios of Tibetan crust was supported by seismic waveform modelling by Rodgers and Schwartz (1998).
文摘以西北农林科技大学校园内生长良好的耐旱树种刺槐(R obin ia p seud oacacia L.)、元宝枫(A certrunca tum Bge.)、沙棘(H ipp ophae rham noid es L.)、白榆(U lm us pum ila L.)、油松(P inus tabu laef orm is C arr.)、白皮松(P inus bung eana Zucc.ex End l.)及中生树种女贞(L igustrum lucidum A it.)和柳树(S a lix m a tsud ana K o idz.f.p endu la Schne id)为研究对象,用压力套在2.5 M Pa下诱导1年生枝条发生木质部栓塞,研究自然条件下木质部栓塞的恢复特性,探讨木质部栓塞恢复特性与PV曲线水分参数间的关系。结果表明,木质部栓塞恢复的快慢,与其小枝的木质部栓塞脆弱性顺序基本一致;栓塞的发生和恢复与树木木质部的结构密切相关。植物木质部栓塞的发生、恢复,与植物耐旱性一样受多种因素控制,虽然与PV曲线水分参数有一定关系,但任何单一水分参数的排序,均与木质部栓塞的脆弱性和恢复速率不完全一致。木质部水势和树木不同部位间的水势梯度是影响木质部栓塞发生和恢复的最主要因素,蒸腾作用、气孔关闭及植物的渗透调节等可能也与木质部栓塞的恢复有关。
