报道了以高分辨力连续可调谐中红外差频激光为探测光源，结合可调长光程怀特池，利用直接吸收的方法探测了CO 2的10011←10002带R支以及部分P支在室温下的水汽加宽吸收光谱。在2 422 cm－1到2 457 cm－1范围内共有26条吸收谱线被探测到，采用Voigt线型对吸收谱线进行拟合，得到了CO 2光谱的水汽加宽系数，结果显示CO 2的水汽加宽系数平均比干燥空气的加宽系数大52%。利用实验测得的CO 2的水汽加宽系数与HITRAN04数据库中CO 2谱线的线位置、线强和干燥的空气加宽系数进行比较，分析了在实际大气中(海平面，10 km光程)不存在水汽和存在水汽(含有2.0 kPa水汽)时该波段CO 2的大气透过率，结果表明潮湿空气与干燥空气之间的最大透过率差约为0.5‰。

Using a high resolution continuous-wave mid-infrared difference frequency generation spectrometer and a long adjustable optical path White cell, water vapor pressure broadening coefficients for 22 transitions in the R branch and last 4 transitions in the P branch of the 10011←10002 band of CO 2 has been detected at room temperature. The recorded lineshapes were fitted with Voigt line profile in order to determine the water vapor collisional broadening coefficients of 26 CO 2 transitions from 2 422 cm－1 to 2 457 cm－1,the result shows that the water vapor collisional broadening coefficients are about 52% bigger than the dry air collisional broadening coefficients. The transmission of CO 2 perturbed by dry and wet air(2.0 kPa water vapor) at the pressure of 0.1 MPa (sea level, optical path of 10 km) has been simulated according to the fitted data from our experiment and the line positions, line intensities and dry air broadening coefficients in HITRAN04 database, and the simulated data show that the largest transmission difference between wet and dry air is about 0.5‰．