Xiong Pan, Gu Xing-Fai, Yu Taol, Meng Qing-Yan, Li Jia-Guoi, Shi Ji-xiang, Cheng Yang, Wang Liang, Liu Wen-Song, Liu Qi-Yuei, Zhao Li-Min
Guang Pu Xue Yu Guang Pu Fen Xi. 2014 Nov;34(11):2953-60.
Detecting oil slick covered seawater surface using the thermal infrared remote sensing technology exists the advantages such as: oil spill detection with thermal infrared spectrum can be performed in the nighttime which is superior to visible spectrum, the thermal infrared spectrum is superior to detect the radiation characteristics of both the oil slick and the seawater compared to the mid-wavelength infrared spectrum and which have great potential to detect the oil slick thickness. And the emissivity is the ratio of the radiation of an object at a given temperature in normal range of the temperature (260-320 K) and the blackbody radiation under the same temperature , the emissivity of an object is unrelated to the temperature, but only is dependent with the wavelength and material properties. Using the seawater taken from Bohai Bay and crude oil taken from Gudao oil production plant of Shengli Oilfield in Dongying city of Shandong Province, an experiment was designed to study the characteristics and mechanism of thermal infrared emissivity spectrum of artificial crude oil slick covered seawater surface with its thickness. During the experiment, crude oil was continuously dropped into the seawater to generate artificial oil slick with different thicknesses. By adding each drop of crude oil, we measured the reflectivity of the oil slick in the thermal infrared spectrum with the Fourier transform infrared spectrometer (102F) and then calculated its thermal infrared emissivity. The results show that the thermal infrared emissivity of oil slick changes significantly with its thickness when oil slick is relatively thin (20-120 μm), which provides an effective means for detecting the existence of offshore thin oil slick In the spectrum ranges from 8 to 10 μm and from 13. 2 to 14 μm, there is a steady emissivity difference between the seawater and thin oil slick with thickness of 20 μm. The emissivity of oil slick changes marginally with oil slick thickness and clearly below that of seawater in the spectrum range from 11. 7 to 14 μm, this spectrum range can be practically used to distinguish oil slick from seawater; Around the wavelength of 11.72, 12.2, 12.55, 13.48 and 13.8 μm, the emissivity of oil slick presents clearly increasing or decreasing trends with the increase of its thickness, which are one of the best wavelengths for observing the offshore oil slick and estimating its thickness.
利用热红外光谱进行溢油检测可在夜间进行,这优于可见光谱;与中波红外光谱相比,热红外光谱在检测浮油和海水的辐射特性方面更具优势,并且在检测浮油厚度方面具有很大潜力。发射率是物体在给定温度(260 - 320 K)的正常温度范围内的辐射与相同温度下黑体辐射的比值,物体的发射率与温度无关,仅取决于波长和材料特性。采用取自渤海湾的海水和取自山东省东营市胜利油田孤岛采油厂的原油,设计了一项实验来研究人工原油浮油覆盖的海水表面的热红外发射率光谱特性及其厚度相关机制。实验过程中,持续向海水中滴入原油以生成不同厚度的人工浮油。通过逐滴添加原油,我们用傅里叶变换红外光谱仪(102F)测量了浮油在热红外光谱中的反射率,然后计算其热红外发射率。结果表明,当浮油相对较薄(20 - 120μm)时,浮油的热红外发射率随其厚度变化显著,这为检测近海薄浮油的存在提供了一种有效手段。在8至10μm以及13.2至14μm的光谱范围内,厚度为20μm的海水和薄浮油之间存在稳定的发射率差异。在11.7至14μm的光谱范围内,浮油的发射率随浮油厚度变化不大且明显低于海水,该光谱范围可实际用于区分浮油和海水;在波长约11.72、12.2、12.55、13.48和13.8μm附近,浮油的发射率随其厚度增加呈现明显的上升或下降趋势,这些是观测近海浮油并估算其厚度的最佳波长之一。