Method for Estimation of Grow Index of Tealeaves Based on Bi-Directional Refl...Waqas Tariq
Estimation methods for grow index as well as total nitrogen and fiber contents in tealeaves based on spectral reflectance and Bi-directional Reflectance Distribution Function: BRDF measurements with ground based network cameras is proposed. Also tea estate monitoring system with network cameras is proposed. Due to a fact that Near Infrared: NIR camera data shows a good correlation to total nitrogen while that shows negative correlation to fiber contents, it is possible to estimate nitrogen and fiber contents in tealeaves with NIR camera data. Through a comparison between actual direct measured and the estimated total nitrogen and fiber contents shows a good correlation so that a validity of the proposed method is confirmed. Also it is found that monitoring of a grow index of tealeaves with BRDF measured with networks cameras is capable. Thus it is concluded that a monitoring of tea estates is capable with network cameras of visible and NIR.
Propagation of Love Waves Through an Irregular Surface Layer in the Presence ...Waqas Tariq
Love waves are surface seismic waves that cause horizontal shifting of earth during the earthquake. The particle motion of Love waves forms a horizontal line perpendicular to direction of propagation. The effect of irregularities present in the surface layer has been discussed in the present paper. The irregularity is in the form of a finite rigid barrier in the surface layer. The surface layer has been assumed to be homogeneous, isotropic and slightly dissipative. The reflected, transmitted and scattered waves have been obtained by Fourier transformations and Wiener-Hopf technique. The numerical computation has been done by taking the barriers of different sizes. The amplitude of the scattered and the reflected waves has been plotted against the wave number. The scattered waves behave as decaying cylindrical waves at distant points. The amplitude of the scattered waves falls off very rapidly as the wave number increases slowly. The amplitude of the reflected Love waves decreases rapidly with the wave number and ultimately becomes saturated which shows that the reflected love waves take a very long time to dissipate making these the most destructive waves during the earthquake.
Webinar: Unwrapping the secrets to holiday success with NostoNosto
Find out how you can tackle your area specific Q4 challenges to succeed during the holiday period and beyond using Nosto. This is a Nosto customer exclusive webinar hosted by our UK & Ireland customer success manager Rabia Qureshi and our Nordics customer success manager Masoud Panshiri.
Method for Estimation of Grow Index of Tealeaves Based on Bi-Directional Refl...Waqas Tariq
Estimation methods for grow index as well as total nitrogen and fiber contents in tealeaves based on spectral reflectance and Bi-directional Reflectance Distribution Function: BRDF measurements with ground based network cameras is proposed. Also tea estate monitoring system with network cameras is proposed. Due to a fact that Near Infrared: NIR camera data shows a good correlation to total nitrogen while that shows negative correlation to fiber contents, it is possible to estimate nitrogen and fiber contents in tealeaves with NIR camera data. Through a comparison between actual direct measured and the estimated total nitrogen and fiber contents shows a good correlation so that a validity of the proposed method is confirmed. Also it is found that monitoring of a grow index of tealeaves with BRDF measured with networks cameras is capable. Thus it is concluded that a monitoring of tea estates is capable with network cameras of visible and NIR.
Propagation of Love Waves Through an Irregular Surface Layer in the Presence ...Waqas Tariq
Love waves are surface seismic waves that cause horizontal shifting of earth during the earthquake. The particle motion of Love waves forms a horizontal line perpendicular to direction of propagation. The effect of irregularities present in the surface layer has been discussed in the present paper. The irregularity is in the form of a finite rigid barrier in the surface layer. The surface layer has been assumed to be homogeneous, isotropic and slightly dissipative. The reflected, transmitted and scattered waves have been obtained by Fourier transformations and Wiener-Hopf technique. The numerical computation has been done by taking the barriers of different sizes. The amplitude of the scattered and the reflected waves has been plotted against the wave number. The scattered waves behave as decaying cylindrical waves at distant points. The amplitude of the scattered waves falls off very rapidly as the wave number increases slowly. The amplitude of the reflected Love waves decreases rapidly with the wave number and ultimately becomes saturated which shows that the reflected love waves take a very long time to dissipate making these the most destructive waves during the earthquake.
Webinar: Unwrapping the secrets to holiday success with NostoNosto
Find out how you can tackle your area specific Q4 challenges to succeed during the holiday period and beyond using Nosto. This is a Nosto customer exclusive webinar hosted by our UK & Ireland customer success manager Rabia Qureshi and our Nordics customer success manager Masoud Panshiri.
Hi
My name is Kiran Aman. My Ms is in Investigative Ophthalmology Ophthalmology and Vision Sciences from University of Manchester. My center of excellence is ophthalmic diagnosis with diagnostic tools
Hi
My name is Kiran Aman. My Ms is in Investigative Ophthalmology Ophthalmology and Vision Sciences from University of Manchester. My center of excellence is ophthalmic diagnosis with diagnostic tools