                           ˿µϣ20141005գ

14.09.30-10.04ûи
14.10.05, ӡϷϵĵ
14.10.05, ӡԪתۣʮ
14.10.05, ƵĿFMר26ڡתܷռƸߵ㡱
14.10.05, ˽۽27ڡʳҰɽзա
14.10.05, ǷٵҪ֤αǰоɹ
14.10.05,  Զ಻ʵ ЦԷ ϸ
14.10.05, ŵ˹ȲǷ2010һƪ¿֤Ĳ໥ģͻûпɹ
14.10.05, xiaojianйʳƷҩƷ춨оԺԺ־NJEMLancetġ
14.10.05, ASEA: µƭ֣
14.10.05, Alexlu۴ԪƱϾѧȥת
14.10.05, ŵȫ淴תһֶķ
14.10.05, ѧԭУǺ꣺תӦڿѧ

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                    Ϸϵĵ

                       ӡ

Ϸϵµ21ͱϵܱΪթϰټҵԪ
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2014.9.30.

(XYS20141005)

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ӡ

1987꣬ûпʼֲתոտʼ飩Ԫ˵
йѾʼתйתԭ磬׼й
ѧҰ䷢ŵʵϣй1992ſʼֲתһ
̲ݣ1997겻֣

(XYS20141005)

˿(www.xys.org)(xys8.dxiong.com)(xys.ebookdiy.com)(xys2.dropin.org)

ƵĿFMר26ڡתܷռƸߵ㡱

http://image.kaolafm.net/mz/audios/201409/6d7518bb-aa3f-434d-af91-00d6b53a0607.mp3

(XYS20141005)

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˽۽27ڡʳҰɽзա

http://v.ifeng.com/fashion/starbaby/201408/01bf5f90-5622-41b6-96a8-b2166025748d.shtml

(XYS20141005)

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ǷٵҪ֤αǰоɹ

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Щ˿йعҺֵһоǷѧ˵˵÷з
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רҵĽǶȿأзǳȱݣ֧ŵQiao_GRL2004 
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ֵģģҲó죬ҲȥоǷġɹ
ĳ嶯ǺǷģ

Fangli Qiao, Yeli Yuan, Yongzeng Yang, Quanan Zheng, Changshui Xia 
and Jian Ma, 2004. Wave-induced mixing in the upper ocean: 
Distribution and application in a global ocean circulation model, 
Geophysical Research Letter, 31: L11303, doi: 10.1029/2004GL019824

˶רҵһϰߣǾǣвĵطͰ
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Yuan, Y., F. Qiao, F. Hua, and Z. Wan (1999), The development of a 
coastal circulation numerical model: 1. Wave-induced mixing and 
wave-current interaction, J. Hydrodyn., Ser. A, 14, 1 C 8.

һˣƪص׾Ȼ
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ǷĵʦԬҵ֡ƪصױǷԬҵ2010
һƪʱ (in Chinese)һƪڿ
ġJ. Hydrodyn., Ser. AӦڿСˮѧоչ
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0 
http://www.qingdaonews.com/content/2006-06/11/content_7038302.htm
1Wave\induced mixing in the upper ocean: Distribution and 
application to a global ocean circulation model
F Qiao, Y Yuan, Y Yang, Q Zheng - Geophysical Research , 2004

2A three-dimensional surface waveCocean circulation coupled 
model and its initial testing
F Qiao, Y Yuan, T Ezer, C Xia, Y Yang, X L, Z Song - Ocean 
Dynamics, 2010

3Modeling effects of tidal and wave mixing on circulation and 
thermohaline structures in the Bering Sea
H Hu, J Wang -  of Geophysical Research: Oceans

4Influences of the surface wave-induced mixing and tidal mixing 
on the vertical temperature structure of the Yellow and East China 
Seas in summer
F Qiao, J Ma, C Xia, Y Yang, Y Yuan - Progress in Natural Science, 
2006

5Effects of the Yellow Sea Warm Current on the winter 
temperature distribution in a numerical model
J Ma, F Qiao, C Xia, CS Kim - Journal of Geophysical Research: , 
2006

6Simulation of double cold cores of the 35 N section in the 
Yellow Sea with a wave-tide-circulation coupled model
X Changshui, Q Fangli, Z Mengning - Chinese Journal of , 2004

7Tidally induced upwelling off Yangtze River estuary and in 
Zhejiang coastal waters in summer
XG L, FL Qiao, CS Xia, YL Yuan - Science in China Series D: 
Earth , 2007

8Improved simulation of the South Asian summer monsoon in a 
coupled GCM with a more realistic ocean mixed layer
Y Song, F Qiao, Z Song - Journal of the Atmospheric Sciences, 2012

9Modeling 1993C2008 climatology of seasonal general circulation 
and thermal structure in the Great Lakes using FVCOM
X Bai, J Wang, DJ Schwab, Y Yang, L Luo - Ocean Modelling, 2013

10Simulation and analysis on seasonal variability of average 
salinity in the Yellow Sea
M Jian, Q Fangli - Chinese Journal of Oceanology and Limnology, 
2004

11Wave-induced mixing in the Yellow Sea
Y Yongzeng, Q Fangli, X Changshui, M Jian - Chinese Journal of , 
2004

12Seasonal variability of thermocline in the Yellow Sea
Q Fangli, X Changshui, S Jianwei, M Jian - Chinese Journal of , 
2004

13A reappraisal of ocean wave studies
Y Yuan, NE Huang - Journal of Geophysical Research: Oceans , 
2012

14Influences of the surface wave-induced mixing and tidal mixing 
on the vertical temperature structure of the Yellow and East China 
Seas in summer
Q Fangli, M Jian, X Changshui - Progress in Natural , 2006

15Analytical estimation of mixing coefficient induced by surface 
wave-generated turbulence based on the equilibrium solution of the 
second-order turbulence closure
YL Yuan, FL Qiao, XQ Yin, L Han - Science China Earth Sciences, 
2013

16Sensitive study of the long and short surface wave-induced 
vertical mixing in a wave-circulation coupled model
C Zhao, F Qiao, C Xia, G Wang - Acta Oceanologica Sinica, 2012

(XYS20141005)

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йʳƷҩƷ춨оԺԺ־NJEMLancet

ߣxiaojian

йʳƷҩƷ춨оԺԺ־N Engl J Med(Ӣҽѧ
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֪ٴоԱӢҽѧ־Ҷ־һƪģ
شΪ쵼־ڶʱ
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ϵĵĵһƪ20133·ҶġImmunogenicity and 
safety of an enterovirus 71 vaccine in healthy Chinese children and 
infants: a randomised, double-blind, placebo-controlled phase 2 
clinical trialҪEV71ٶͯӤ2ٴʵ飬
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˾йʳƷҩƷ춨оԺ־

ϵĵĵڶƪ20136·ҶġEfficacy, safety, and 
immunology ofan inactivated alum-adjuvant enterovirus71 vaccine in 
children in China:a multicentre, randomised, 
double-blind,placebo-controlled, phase 3 trial.Ҫ
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ɽֺһڣ EV71 Ⱦµڲıʴﵽ 90%
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ţͨѶ߷ֱţйʳƷҩƷ춨оԺۺй
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ϵĵĵƪ͵ƪ20142·Ӣ־ġAn 
Inactivated Enterovirus 71 Vaccine in Healthy Children 
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ԤٴоٳɣͨѶйҽѧѧԺҽ
ѧѧойʳƷҩƷ춨оԺ־

ͬһһƪġEfficacy, safety, and immunogenicity of an 
enterovirus 71 vaccine in China й71Чԡ
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ĵһ߽ʡĸţͨѶǱƷ
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(XYS20141005)

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ԭһϲӣൺҾҵͺϲ
ҲϲѧʦԺʿˮƽߡ

4û˵۵һû˵Ǿߵ˳
ͶʱȷģйˣԾַܳԺҲŷĩ
ҲܱԹ̫ܹˡ

Ҳڳʶңֻ˵ڷԻܡ

һƪ£һƪޱ𣬵ʵֻáˡظ

ٲʵû㣡

2. Ҷ

ܺã̬Ҳ棬һ£

´ʵҲٻشˣлл

1ȡֵΪ1ǾԤҪϸҪ۲⣬̶ֳȵĽ
ƣܳìܡ

2֪POMȷȽϣûµģʽúáǣ
ִģʽҲȷٴڻϲ⣬֮йKPP


ϣɻаٴθлɣʵлл

3. 1ϷߣǷǵ北

۲ҪþСֻɻһŶӸɵģм
г룬ûвʵΪ˰ҴˣҵĹͲ
õϰɣ

ٴǿ

 Զ಻ʵ ЦԷ ϸ

һʵɣ棡
ûйԣǻʧȥʵģ
:-P

(XYS20141005)

˿(www.xys.org)(xys8.dxiong.com)(xys.ebookdiy.com)(xys2.dropin.org)

Ƿ2010һƪ¿֤Ĳ໥ģͻûпɹ

ߣŵ˹Ȳ

ṩһϣԲ֤һ˵Ƿֱڶû
໥ģ͡ĸòϵ˵

Ƿƪ2010귢ģ¼һıǡģ
ĳԡɼֱ2010ֻڳԣ2003Ѿ
ӵСȻԡݱʶڲ˱ϣҲǼٵġ

ݿǷзƺ뷢һʵʹܵĲ໥
ģͻһξ롣̸˼·ϡ˼·Ǵǰ
궼һ̸ֱҲˡƪµصȻǿյ
Ҫԡĳ˸ݣֻQiao_GRL_2004档ı
ģϵͳͳԣ͹Ӧûںģͺͺģ
֮󣬶Աģʱĵģõĺ˺ͺʲ
ôĽٻͬʱᵽͺ˵ĽȻĸûἰ˵Ľ
һϵеĶͬص㡣

໥ģͲҪǡ״໥ۡз
Եĺѧ2005ͷһƪǵĲ
໥ģͣ¼ѧߵʵõĺ
˵Ľ

ݱʶڲ˱ϣǷǿתֻһ˹
ٺģͣPOM⼸ķ˲٣˵ǿ
ɫĲ໥ģõʵʾġĽʵʶ
ǡȫֹĽӡǲûв໥ģͣPOMģ
ӵνյĻǿҲϸذQiao_GRL_2004еı
ʽPOMģͣ׳ġ


¼һǷ
ѧڿOcean Dynamics (2010) 60:1339C1355
ı⣺A three-dimensional surface wave-ocean circulation 
coupled model: System description and initial testing
ߣF Qiao, Y Yuan, T Ezer, C Xia, Y Yang, Z Song
ժҪ
A theoretical framework to include the influences of nonbreaking 
surface waves in ocean general circulation models is established based 
on Reynolds stresses and fluxes terms derived from surface 
wave-induced fluctuation. An expression for the wave-induced viscosity 
and diffusivity as a function of the wave number spectrum is derived 
for infinite and finite water depths; this derivation allows the 
coupling of ocean circulation models with a wave number spectrum 
numerical model. In the case of monochromatic surface wave, the 
wave-induced viscosity and diffusivity are functions of the Stokes 
drift. The influence of the wave-induced mixing scheme on global ocean 
circulation models was tested with the Princeton Ocean Model, 
indicating significant improvement in upper ocean thermal structure
and mixed layer depth compared with mixing obtained by the Mellor
CYamada scheme without the wave influence. For example, the modelC
observation correlation coefficient of the upper 100-m temperature 
along 35 N increases from 0.68 without wave influence to 0.93 with 
wave influence. The wave-induced Reynolds stress can reach up to about 
5% of the wind stress in high latitudes, and drive 2C3 Sv transport 
in the global ocean in the form of mesoscale induced mixing is more 
pronounced in middle and high latitudes during the summer in the 
Northern Hemisphere and in middle latitudes in the Southern Hemisphere.



¼ѧߵ
ѧڿOcean Modelling Volume 8, Issue 3, 2005, Pages 203C236
ı⣺Impact of a coupled ocean waveCtideCcirculation system 
on coastal modeling
ߣl-Ju Moon
ժҪ
The impact of a coupled ocean waveCtideCcirculation system on 
coastal modeling for wind waves, oceanic circulation, and water-mass 
simulation is investigated by coupling of two well-tested models: the 
third-generation wave model (WAVEWATCH-II) and the Princeton ocean 
model (POM). In this study, several numerical experiments in the 
Yellow and East China Sea (YECS) are performed for the ideal winter 
case and the typhoon Winnie case. In the coupled system, wind waves 
are influenced by both currents and sea level elevation induced by 
tides, storm surges, and oceanic circulation. Tides were the most 
influential factor in modulating mean wave characteristics in the YECS. 
The magnitude of the modulation of mean wave parameters at neap tides 
is found to be half that at spring tides. In the YECS the tides affect 
not only wind waves, but also seasonal circulation and water-mass 
distributions. Tides increase the bottom friction of the YECS 
significantly and this contributes to a change of winter current 
direction up to 60 C in the YECS and a decrease of surface 
temperatures along the trough of the Yellow Sea up to 4 C in winter. 
Tides in summer produce the strong vertical mixing in shallow regions. 
This leads to the formation of tidal fronts in a boundary between 
well-mixed and stratified regions and causes sea surface temperatures 
(SST) along the west coast of Korea decrease as much as 3 C. Effects 
of ocean waves on coastal circulation and SST simulations are 
investigated considering wave-dependent stress, wave breaking 
parameterization, and Langmuir circulation under typhoon Winnie 
conditions. The results show that the wave-dependent stress, which is 
strongly dependent on wave age and relative position from storm center, 
as well as the wave breaking have the most significant impact on the 
SST distribution.

(XYS20141005)

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ASEA: µƭ֣

ӣ һѧϰĲʿΪϲܣ˽
һֺܹ˶ϣASEAעĳɷ־κˮˮ˵
Ǿκˮ˵˶30%ϡһĹ˾
ϵһЩۣоƭ˵ģ

http://www.sciencebasedmedicine.org/asea-another-expensive-way-to-buy-water/

ǵ˶ʵоɱѧDavid Niemanʵҽ
УNieman˶ҽѧϯۺܶ࣬˵ʵ
֤ˮǿˮ֤α

Ĺ˾ҳѾ۵ŷޣ֪û˵йۣǰ
Сµƭ֡

(XYS20141005)

˿(www.xys.org)(xys8.dxiong.com)(xys.ebookdiy.com)(xys2.dropin.org)

۴ԪƱϾѧȥת

ߣAlexlu

ҵ̲ס״λ

Ҹоʱб

ϴĸѧļݲӦýһżϡ
ԤгǷ㹻ļֵʲôֻҪ۽
ڿɿ֤ݺܵ߼֮ϣֵ÷̽֡
ǽľˮԪڱЩΪûѧ
ѧ﷢ۣ߶ԴѧȽ֪ʶʹûκ洦
Ǳѧģô˻ѧĲκƷζ

ǸϴѧһֵĻᡣǼǧҥԺһ
ǵͣϵӰҲϴֳ֤Ĵͳָ
Ƚ˵壬ɴ˲ЧӦɨ൱һִɵĸЧ
Ҳϴ˵ۡ

֮ܶһ仰ǲܸıĳЩŻʦ˼άʽܱ
Լ̬Ⱥͼֵ

(XYS20141005)

˿(www.xys.org)(xys8.dxiong.com)(xys.ebookdiy.com)(xys2.dropin.org)

ŵȫ淴תһֶķ

ߣRich Roberts

ÿ궼ȥУеΪû㹻ʳԣе
ΪԽʳȱزٵӪء˿ڵӣЩ⽫
ԽԽءǣЩͽ౾ǿԤģҲ
˵ǿӦִѧͨӪԽġõĹؼ
ֲ֣оͰתִŴѧܹµ
תƷ֣ʹũõߣʹũҲܹǰ
ķϵƶΪҪǣ߳Ӫɷ֡
תѾ൱죬صʵҶܹؼ
áȻЩѧ˵׵һȴΪȫ
綼ڼ۵Ļ⡣ΪʲôЩũûбӹ㷺ؼӦ
ãЩչйңЩƷֱпʵʵڵظǵ
ġΪʲô˾Ҫɿڻһת

ȣǱʲôתԴũҵǵ
һֱڲֲͨͬƷ֮ӽ߲Ӫֵ
ũֲֲӽֲִӽ˵Ƚס
ǣӽ״˵Ƿǳ޵ġΪ
һ˵ȡǷܹԵϵԶȴȻܹӽֳЩֲ
ҵҪ״Ϊתַĳͻƣ
ּͨDNAûԵϵֵĻתƵֲ֮С
ҪǣѾĳҪ״ĳһĳתƵһ
ֲУǲԵֲﵱȥѰǸ򣬻Եκﵱ
ȥѰңҪ״Դ⣬ּתƻľ׼
ǰļġôͳַһתƵһ
Ļǳǧϰٸͨ޷֪ЩԡȻ
DNAķ֣תƵֻ֪ĳЩضĻҪرָ
ǣʹʲô˵ʲôֶתƻõֲȫ
£ҪõĽõũﰲȫǲȫ
׿ͽߵķ롣鼼Ҫһ
һˮƷϵתƵ˵һƷϵõıתˮõ
ͳַõı㲻תˮֵǣDNAַ
תƻľ׼ȷǳߣΪҪäĿؽٸһ
תƵһΣգʵ㣳ʶ߼˵תũ
ʳй㷺ļſԷʳõĻôڴͳũʳ
ҲӦˡ

ʵΧתΪʲôⳡ۵ԭ򣬻شʵʮּ򵥣
Ρ֮ͨԶִũҵۺҵкܴǣΪ
ǻûʶִܸõũ̲صļֵڷ
չйңһЩͨΪĿĶ𷴶ת˶
ǸҪ͸Ӫʳַ
ת˶ɵ˼ҶЩҿ϶һǱڵѡ
ԭͬŷ޹ҲȡǳǿӲķתйء20
90ڣɽһҿũҵ＼˾һЩũҵۺҵ
ͼתŷ޵ũӦ˵ǷһܴսԴ
Щ˾ɽû뵽ǵҵᱻΪһ
˾ͼ¢ŷ޵ʳ﹩Ӧŷ˵ǿҷԡɽ
๫˾ŷ޾Ӫҵ񣬺Ѹ¼˵ɽ˾һҲ
˾

ôܹɽ˾¢ŷʳ﹩Ӧͼ
ֹвأ취ǲȥɽ˾ӶԵҵ
ṩĲƷָЩƷоת
ʹõķûоԣпΣɫ֯һЩ
ȡֲԿǷǳɹģҪŷ˴һ¼ܻ
ɵľ޴Σȳܵ¼Σпʧȥ
ϣֲԸЧԣǵѡ
ȻѡƱ

УѾЩת˵һƲ⣺һ
ĳһνġѧĹŹʳŷ˵ʳǾпܶ
ǵĽӰ졣ˣǿǷпܵ
ѵļµͼǣΪ˰ȫΪЩʳӦܵϸܺ
ϸԵĺͺǣת˶ܿȫʧأ
ЩӸɴҪȫֹתǳϴȡ
ָͨͨĿţҪдδйķǳϸļܣ
ڳɹֹתŷޡŷ˵ִʲ
ô⣬Ϊȫŷ޺ͱķܹͨʳ﹩
Լ˿ڻи࣬ǲչйҪתˣ
תͱ㷺ӦũĲѾվ˽Ÿ

ôأԭɫ֯ŷ޼̰ת
ǻǵ˶㵽˹⣬߷չйҵҲӦ
ֹתϾסڷչйҵ˵תŷǸ
Ȼ㲻طǰȫġ⻹Զֹڴˡŷ
޺ط˶ûиԣ㹻ǮʳҲз
ʳ﹩ǵҪŷ޺Ӫʳ洦ɵã
ҴҶ𡣿ڷչйȴȫ޹ҡ
ӡȴδ½ԼƶңЩطʳѷ
ʳ﹩㣬ʳȱزٵӪءʮ
Ϳµĸǿάֲʳȴ
ǵļͥΪֲũƷ̫鷽ǵ
ũԸĽߣһͺԡӪԼ
ԡǣֹתĻͲƷ֡
ŷ޵ͺνɫ֯һַǳΣյϷܻܿʹ
ʮ˰ڻѵʱˡӦóϣⲻڼ
ǺµǴũҵۺҵҪǲƷǵķ

ⷽһܺõӣǡƽ(1218.90, 3.50, 0.29%)ˮ
1999꣬λѧӢ?˹ͱ˵?ݶ±˵
ɹһܹϳɦºܲصˮƷϵºܲǺϳάAĲ
ϡ֮ҪתˮΪԴΪʳ
άAȱ֢ȱάAʧͰڵķȱݣ
пܵزۻһʹࡣȫÿһٶͯάAȱ֢
иһܾĥƽˮṩԸֲĸũ
֡ʳֻƽˮܹһɳеĶͯά
AҪƽˮŷɹģܵϸŷ޷
ѹƣڷչйֲȻ˸еģΪת
ɫһֱŷתֱ׳
ѹηηţתڹҲҪܵصƣ
ڻƽˮҲδһط׼ҵֲŷ޷ת
ķЧֹ־ũƹ㣬԰Ƶ
ˣд󲿷ǶͯڻάAȱֱ֢ļ
ȥѸ˭أ

ҿӦùνġɫ֯ϵļӣ
Ǻ˵תʳƷΣĽӦֲŷ޵ЩԺ
˵ţ˿ѧѾͨһЩδйϸʵ֤Щתũ
ǰȫģҲΪƲѧҷ˴оĶת
ȫԽѧ֤ͬʱȴûκһֵĿѧоָ
ЩʳΣյġ

ϵÿһҿѧо۹ҿѧԺǶоһ
⣬ܹ֤תȷʵȫɿûκһҹҿѧԺκһ
Ŀѧоͬתڱôͳַ
ͬĹ۵㣬⵱Ȼǲ޵ġЩתũﱾ
Σաڹȥ5000еũҵиıȻ
κʳûκβͬȻתõķҲ
˵ǰδʹù·ǣֻǶس
ֲͶЩһָĽѡ·Ĳ̱κ
Σա

תʳƷϡΣաʶ޿ѧݡ
ΣշһЩϵļӾۼͼֹԵļ츣
ࡣЩũҵĺȣʹطܾ񷢴
ʳﱣϣӦΪ˸ֱӺͼΡɴˣǲò
ۣǷӰԶķ

йñ桷Լ༭ٻ룩

.޲(Rich Roberts)1993ŵҽѧѧߣ
ѻRNAзֵı,ܳķѧ֮һܳ
ĿѧɾͣӢŮ׷ΪӢʼҾʿ,ѡӢʼҿѧԺԺʿ

޲ĿüݷȺӣڡѧȻ
ڿ230ƪѧġ޲Ĳʿ쵼Ӣʵ
(NEB˾)1974꣬ƿҵںϡ

ΧתʳƷۣȫΧڶһŻ⣬йͬ
ˣһЩ۵Ļҩζ㡣Ϊˣйñ桷
޲רã޲ĲʿԴ˻ר׫ģһ


(XYS20141005)

˿(www.xys.org)(xys8.dxiong.com)(xys.ebookdiy.com)(xys2.dropin.org)

ѧԭУǺ꣺תӦڿѧ

ǺϵֲѧҺԭѧУҲйѧԺ
ԺоԱShanghai Daily ڽշ߲ɷǺڱGM 
debate needs grounding in science

Qתȫģ

AתѾ㷺ֲ20ꡣ1996״ֲʼȫ
緶Χתֲ100ֹ2012Ѿﵽ1.7ڹ꣬
йũ1.4

Ƕת۵һ£תﻹǵõѸӦáת
ӦùȥҪڱԽԽķչйӡȡͰ
͢ҲһСйȥڶλѾҳԽ(
עйתֲĿǰλ͢ӡȡô֮
ӵλ)

ݹũҵ＼Ӧ÷֯(ISAAA)ƣֲУȫ
81%ϵĴ󶹣64%޻29%׺23%Ͳ()ת
ӡ

ȫĿǰֲת29Һ͵ѾʼתƷ
ҵԼ95%Ĵ󶹺75%ת(עũҵ
ݣ 2014תռʴ93%)Ѿŵ׼
о֤޺

ⷽŷ޽ΪأתһЩұֲŷɽ
ȹѻʽ׼תƷȫΧתũҵһֱ
ơ

Qʣתǰȫ𣿡Դô

AۡתֲǷǰȫû壬Ӧþ尸
򹤳̼Եģȫȡ޸ʲôӽͨ
ҲתǷȫȡתضʲôá

磬Bt浰й㷺Ϊסʵ಻
ͬBt֡Ƿֱרŵɱͬ͵档ɱBt׶
ӻӬЧ˵á

Btױ뵽ת󶹺СΪ˻жԣѧ
˴оͲԡ𹫲ĲԽʾ
һʳ200תMON 810(עɽ˾һ
תƷ֣Ŀǰ6׼ֲԼ20ұ׼ʳƷ)ĴBt
ȻǰȫģҲû֤ݱ˺ǵֳϵͳǺܶ˶
֪ЩԼƲݿ֤ѱ׼ת
ǰȫģ֪õҵЩݡЩݵĺʲô

Qֻ֧򷴶תô

Aת򲻽й綼顣йѧԺֲ
ѧ̬ѧоԼйֲѧѧÿ궼ֲվٰ
ڽֲѧתȡЧ

й˿ڶ࣬ǶͬһвͬĿؼӦð
ۻ۽ڿѧԵĻϣǽλ

һЩýתħΪʲôܶڵĿѧ
Ը֧ۡת/ϡ顱ıǩ
һЩƣת񣬻֡ܲ1966
1976ꡰĻзֻ֧򷴶ڲͬԭŷ޶ת
ֵ÷ǳأǻڿѧݺ֤ݵġ

£תԽ⡣ľϻ߲ܸľϴ
Եƻɱáֲɵƻ10ʹľϲ
90%ϣӶݻļȫľϲҵвԵת
ľûбзǽͿܳԲľˡ

תﲻпԻͳݼԣδ԰ݸҪĽ
ɫѧڽоΪСͺλ

QתԻв

AתһҪĻЧǿԴũҩʹá
ȥ10ڹ㷺ֲתũҩʹ١йҲһ
й޻ũҩصֲת޻ɱ
ʹѾ½80%

йÿĵũҩͻʳȫ֮ܲһйĸ
СйʹɱͻѧϡйũҵȾռ
ȫȾһ롣

ˣũҩʹǸƻЧ;

ѧڽзҪٷϵĸЧ̵δϵʹҲ
١

ʵǸδ仯ͼȫƽ1
϶ȣҪũ½10%һЩӦδ
˵̫ˡ򹤳̿԰ǿԸõӦ
ũһЩǱҰָõΪǵδ

QйתʳҵӦ÷ȷ·߻ƻ

Aܵ˵йתķչȲǰҲܵһЩ
صӰ졣ת޻йȡ˾޴ɹ

1980ĩΣʹй޻һ룬ɱ
á

ʱѧҿBt޻档ɽ˾ͼ似
ߵļ۸۸ййѧǿչԼо֮й
Bt޻

й80%޻ǻԼ＼ûԼ
ôǾͻᱻ˾ƣӡȡӡȵ޻ֲ
תûԼרΪʲô˾

תһֱһĻ⣬ʳƷȫ򻷾ȫҪ
һĿѧۡΪʲôڴתӦҪϸ
׼

йתĹҪϿ

һ˾תİȫ֤飬͵ڱ׼
ˡйڻðȫ֤˾ҪļƷ֤
飬ũӹ֤;Ӫִգֲƹ㡣ҵʿҪ
ʱ̡

תʳӦãȻûȷ·ͼйû֪
ðȫ֤ȡתʳӪִաⷽ沢ûȷĹ涨

йеתBt򿹳ˮƷֺһתֲøƷֵİȫ
֤Ѿڡû֪һôƶҵƹӦá

һЩӹ˾Ͷ˴ʽзڵܻώ
ǵ顣ûȷ·ͼ˾ͲƽûͶ
룬Ҫ֪ҵתоԼӦϷŹؼá

ҿתĹԺϸ񣬵ҪĿǰйת
ƹӦѾΪһ⡣

(XYS20141005)

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