Ku-band long distance site-diversity (SD) Characteristics using new measuring system

Abstract—This paper deals with the short (10 km) and long dis-tance (300–1400 km) site-diversity (SD) characteristics by using a newly developed measuring system. In the proposed measuring system, six earth stations transmit 14-GHz band QPSK signals, and one measuring earth station receives 12-GHz band signals and processes them to determine SD characteristics. As a result, easy operation and maintenance, low-cost measuring system construc-tion and highly accurate data have been obtained. By comparing those measured results with the SD joint probability approxima-tion equation in ITU-R Rec.P.618-7, a good agreement can be ob-tained. Furthermore, the effect of typhoons on SD characteristics were measured. Index Terms—Rain attenuation, satellite communication system, site-diversity (SD) measurement system, SD characteristics, VSAT system design. I

Lingual nerve stimulation-induced c-Fos expression in the trigeminal spinal nucleus

The aim of the present study was to investigate whether electrical stimulation of the unilateral central cut ends of the lingual nerve produces trigeminal-parasympathetic reflex vasodilatation in both sides of the lower lip and stimulates neurons in the trigeminal nuclear complex in rats subjected to cervical vagosympathectomy, deeply anesthetized with urethane and artificially ventilated. Immunohistochemical detection of c-Fos expression was used to assess the impact of prolonged lingual nerve stimulation. We found that unilateral lingual nerve stimulation at 10min intervals for 200min produced the following: (1) consistent blood flow increases predominantly in the ipsilateral side of the lower lip, (2) more profound expression of c-Fos protein ipsilaterally in all subnuclei of the trigeminal spinal nucleus (Vsp) except the trigeminal subnucleus oralis, (3) a greater number of c-Fos-positive neurons in the ipsilateral trigeminal subnucleus interpolaris/caudalis transition zone (Vi/Vc) compared with the four other areas (trigeminal subnucleus caudalis/upper cervical spinal cord transition zone, subnucleus caudalis, subnucleus interpolaris, and subnucleus oralis) of the Vsp, and (4) no statistically significant increase in c-Fos expression in all subnuclei of the Vsp of the contralateral side in comparison with the control rats. The present studies and our previous data suggest that impulses elicited by electrical stimulation of the lingual nerve converge on the ipsilateral Vi/Vc in the Vsp and that the parasympathetic vasodilator neurons and salivatory nucleus, after receiving projections from the Vi/Vc in the Vsp, project to the lower lip via the otic ganglion

High-resolution seismic reflection profiling across the surface rupture associated with the 2004 Mid-Niigata Prefecture earthquake, central Japan : data acquisition and processing

The 200.4 Mid-Niigata Prefecture earthquake (Mj 6.8) generated surface ruptures along the eastern rim of the Uonuma hills. To reveal the relationship between a seismogenic source fault and surface ruptures, shallow, high-resolution seismic reflection profiling was undertaken across the surface ruptures and the active faults. The seismic source was a mini-vibrator and seismic data were recorded by a digital telemetry system. The source and receiver interval was 10 m4 The seismic data were processed using conventional CMP seismic reflection methods. The resultant depth-converted seismic section portrays an emergent thrust beneath the surface rupture associated with the Mid-Niigata Prefecture earthquake

High-resolution seismic reflection profiling across the Shiraiwa fault, eastern margin of the Yokote basin fault zone, northeast Japan : data acquisition and processing

The eastern margin of the Yokote basin fault zone extends about 56km at the western foot of the Ou Backbone Range, northeast Japan. The Rikuu earthquake (M=7.2) occurred in the Ou Backbone Range (Mahiru Range) on 31st August, 1896. Associated with this earthquake, four thrust faults-Obonai, Shiraiwa, Ota, and Senya fault3 appeared on the surface of the western foot of the Mahiru Range. These faults were highly sinuous with numerous gaps and en echelon steps. We conducted a high-resolution seismic reflection profiling survey across the Shiraiwa fault. The obtained seismic reflection data were processed by conventional common mid-point methods, post-stack migration, and depth conversion. The subsurface structure across the Shraiwa fault is characterized by branched low-angle reverse faults and conjugate back-thrust. The emergent thrust associated with the 1896 earthquake is regarded to be a subsidiary reverse fault