红外与激光工程
紅外與激光工程
홍외여격광공정
INFRARED AND LASER ENGINEERING
2014年
3期
737-741
,共5页
田昌会%蔡明%杨百愚%范琦%王斌科%王伟宇%屈绍波
田昌會%蔡明%楊百愚%範琦%王斌科%王偉宇%屈紹波
전창회%채명%양백우%범기%왕빈과%왕위우%굴소파
红外辐射%星载探测%对比度
紅外輻射%星載探測%對比度
홍외복사%성재탐측%대비도
infrared radiation%satellite-borne detector%contrast
推导了星载红外探测在地面、大气双背景下探测器处的辐射照度对比度计算公式,计算了目标在不同温度、不同高度的目标与背景的绝对对比度和相对对比度。分析指出:随着目标温度、高度增加,在波长大于2.5μm区域绝对对比度与相对对比度相应增大,目标高度越高,同等距离下对比度随目标高度的变化越小;波长小于2.5μm需考虑太阳的影响;当目标在0 km高度时,2.9~4.1μm波段为最佳探测波段,随着目标高度的增加,可用探测波段范围增大,峰值波长向短波方向微移,当目标高度大于10 km时,相对对比度峰值在2.6~2.8μm之间;距离地面越近,大气对红外辐射的衰减越大。
推導瞭星載紅外探測在地麵、大氣雙揹景下探測器處的輻射照度對比度計算公式,計算瞭目標在不同溫度、不同高度的目標與揹景的絕對對比度和相對對比度。分析指齣:隨著目標溫度、高度增加,在波長大于2.5μm區域絕對對比度與相對對比度相應增大,目標高度越高,同等距離下對比度隨目標高度的變化越小;波長小于2.5μm需攷慮太暘的影響;噹目標在0 km高度時,2.9~4.1μm波段為最佳探測波段,隨著目標高度的增加,可用探測波段範圍增大,峰值波長嚮短波方嚮微移,噹目標高度大于10 km時,相對對比度峰值在2.6~2.8μm之間;距離地麵越近,大氣對紅外輻射的衰減越大。
추도료성재홍외탐측재지면、대기쌍배경하탐측기처적복사조도대비도계산공식,계산료목표재불동온도、불동고도적목표여배경적절대대비도화상대대비도。분석지출:수착목표온도、고도증가,재파장대우2.5μm구역절대대비도여상대대비도상응증대,목표고도월고,동등거리하대비도수목표고도적변화월소;파장소우2.5μm수고필태양적영향;당목표재0 km고도시,2.9~4.1μm파단위최가탐측파단,수착목표고도적증가,가용탐측파단범위증대,봉치파장향단파방향미이,당목표고도대우10 km시,상대대비도봉치재2.6~2.8μm지간;거리지면월근,대기대홍외복사적쇠감월대。
The irradiance contrast formula of target and background for satellite-borne infrared detector under both ground and atmosphere background was derived. The absolute contrast and the relative contrast at various target altitude and temperature were calculated. The analysis conclusions show that the absolute contrast and the relative contrast increase with the target temperature and altitude for wavelength of larger than 2.5μm. The higher the target altitude is, the less the contrast changes per unit distance. The effect of the sun should be considered when the wavelength is less than 2.5μm. For target at 0 km altitude, 2.9-4.1μm is the optimum detective waveband. As the target altitude increases, the available detective waveband broadens and the peak wavelength moves to short wave direction slightly. When the target altitude is higher than 10 km, relative contrast peak value appears at 2.6-2.8μm. The nearer the target is from the ground, the higher the atmospheric attenuation is to infrared radiation.