半导体学报
半導體學報
반도체학보
CHINESE JOURNAL OF SEMICONDUCTORS
2005年
3期
429-435
,共7页
双栅MOSFET%一维解析量子求解%沟道深度方向的非均匀电势%电子密度%阈电压%沟道深度
雙柵MOSFET%一維解析量子求解%溝道深度方嚮的非均勻電勢%電子密度%閾電壓%溝道深度
쌍책MOSFET%일유해석양자구해%구도심도방향적비균균전세%전자밀도%역전압%구도심도
DG MOSFET%1D analytical QM solution%non-uniform potential in channel-depth direction%electron density%thresholdvoltage%channel depth
推导了双栅MOSFET器件在深度方向上薛定谔方程的解析解以求得电子密度和阈电压.该解析解考虑了任意深度情况下沟道中深度方向上电势的不均匀分布,结果与数值模拟吻合.给出了电子密度的隐式表达式和阈电压的显式表达式,它们都充分考虑了量子力学效应.模型显示,在亚阈值区或者弱反型区,电子密度随深度增加而增加;然而,在强反型区,它与深度无关,这与数值模拟的结果吻合.结果进一步显示,只考虑方形势阱的量子力学结果,略高估计了阈电压,且低估了电子密度.误差随着深度的增加或者栅氧厚度的减少而增加.
推導瞭雙柵MOSFET器件在深度方嚮上薛定諤方程的解析解以求得電子密度和閾電壓.該解析解攷慮瞭任意深度情況下溝道中深度方嚮上電勢的不均勻分佈,結果與數值模擬吻閤.給齣瞭電子密度的隱式錶達式和閾電壓的顯式錶達式,它們都充分攷慮瞭量子力學效應.模型顯示,在亞閾值區或者弱反型區,電子密度隨深度增加而增加;然而,在彊反型區,它與深度無關,這與數值模擬的結果吻閤.結果進一步顯示,隻攷慮方形勢阱的量子力學結果,略高估計瞭閾電壓,且低估瞭電子密度.誤差隨著深度的增加或者柵氧厚度的減少而增加.
추도료쌍책MOSFET기건재심도방향상설정악방정적해석해이구득전자밀도화역전압.해해석해고필료임의심도정황하구도중심도방향상전세적불균균분포,결과여수치모의문합.급출료전자밀도적은식표체식화역전압적현식표체식,타문도충분고필료양자역학효응.모형현시,재아역치구혹자약반형구,전자밀도수심도증가이증가;연이,재강반형구,타여심도무관,저여수치모의적결과문합.결과진일보현시,지고필방형세정적양자역학결과,략고고계료역전압,차저고료전자밀도.오차수착심도적증가혹자책양후도적감소이증가.
The analytical solutions to 1D Schr(o)dinger equation (in depth direction) in double-gate (DG) MOSFETs are derived to calculate electron density and threshold voltage.The non-uniform potential in the channel is concerned with an arbitrary depth so that the analytical solutions agree well with numerical ones.Then,an implicit expression for electron density and a closed form of threshold voltage are presented fully comprising quantum mechanical (QM) effects.This model predicts an increased electron density with an increasing channel depth in subthreshold region or mild inversion region.However,it becomes independent on channel depth in strong inversion region,which is in accordance with numerical analysis.It is also concluded that the QM model,which barely considers a box-like potential in the channel,slightly over-predicts threshold voltage and underestimates electron density,and the error increases with an increasing channel depth or a decreasing gate-oxide thickness.