USDA, ARS Biological Control of Pests Research Unit, PO Box 67, Stoneville, MS 38776, USA.
J Insect Sci. 2008;8:1-12. doi: 10.1673/031.008.3101.
A study was undertaken to characterize surface temperatures of mounds of imported fire ant, Solenopsis invicta Buren (Hymenoptera: Formicidae) and S. richteri Forel, and their hybrid, as it relates to sun position and shape of the mounds, to better understand factors that affect absorption of solar radiation by the nest mound and to test feasibility of using thermal infrared imagery to remotely sense mounds. Mean mound surface temperature peaked shortly after solar noon and exceeded mean surface temperature of the surrounding surface. Temperature range for mounds and their surroundings peaked near solar noon, and the temperature range of the mound surface exceeded that of the surrounding area. The temperature difference between mounds and their surroundings peaked around solar noon and ranged from about 2 to 10 degrees C. Quadratic trends relating temperature measurements to time of day (expressed as percentage of daylight hours from apparent sunrise to apparent sunset) explained 77 to 88% of the variation in the data. Mounds were asymmetrical, with the apex offset on average 81.5 +/- 1.2 mm to the north of the average center. South facing aspects were about 20% larger than north facing aspects. Mound surface aspect and slope affected surface temperature; this affect was greatly influenced by time of day. Thermal infrared imagery was used to illustrate the effect of mound shape on surface temperature. These results indicate that the temperature differences between mounds and their surroundings are sufficient for detection using thermal infrared remote sensing, and predictable temporal changes in surface temperature may be useful for classifying mounds in images.
一项研究旨在描述进口火蚁蚁丘(膜翅目:蚁科)及其杂种 Solenopsis invicta Buren 和 S. richteri Forel 的表面温度特征,因为这与蚁丘的太阳位置和形状有关,以更好地了解影响巢丘吸收太阳辐射的因素,并测试使用热红外图像远程感知蚁丘的可行性。蚁丘表面温度的平均值在正午后不久达到峰值,并超过了周围表面的平均表面温度。蚁丘和周围地区的温度范围在正午附近达到峰值,而蚁丘表面的温度范围超过了周围地区。蚁丘和周围地区之间的温差在正午左右达到峰值,范围约为 2 到 10 摄氏度。与每天时间(表示为从日出到日落的日照小时的百分比)相关的二次趋势解释了数据变化的 77%至 88%。蚁丘不对称,平均顶点向北偏移平均中心 81.5 +/- 1.2 毫米。南面临面比北面临面大约 20%。蚁丘表面的方位和坡度影响表面温度;这种影响受时间的极大影响。热红外图像用于说明蚁丘形状对表面温度的影响。这些结果表明,蚁丘和周围地区之间的温度差异足以通过热红外遥感进行检测,并且表面温度的可预测时间变化可能有助于对图像中的蚁丘进行分类。