Some Instruments Used by Division 10, NDRC at Dugway Proving Ground for Continuous Recording of Micrometeorological Conditions

1945 ◽  
Author(s):  
S. W. Grinnell
Keyword(s):  
Continuous Recording ◽  
Micrometeorological Conditions

Continuous recording of pyloric sphincter pressure in dogs

1985 ◽  
Vol 30 (7) ◽  
pp. 669-674 ◽  
Author(s):  
Carlos C. Defilippi ◽  
Elsa Gomez
Keyword(s):  
Pyloric Sphincter ◽  
Continuous Recording ◽  
Sphincter Pressure

Continuous recording of hand position in the study of complex visuo-motor tasks

1973 ◽  
Vol 11 (1) ◽  
pp. 123-125 ◽  
Author(s):  
C. Prablanc ◽  
M. Jeannerod
Keyword(s):  
Continuous Recording ◽  
Hand Position ◽  
Motor Tasks

A device for the automatic, continuous recording of stereoscopic visual acuity

1970 ◽  
Vol 25 (4) ◽  
pp. 115-123 ◽  
Author(s):  
C.E.T. Krakau
Keyword(s):  
Visual Acuity ◽  
Continuous Recording

A seismic investigation of crustal structure in the Western Transvaal*

1952 ◽  
Vol 42 (1) ◽  
pp. 53-80
Author(s):  
P. L. Willmore ◽  
A. L. Hales ◽  
P. G. Gane
Keyword(s):  
Crustal Structure ◽  
Intermediate Layer ◽  
Continuous Recording ◽  
Travel Times ◽  
Local Anomaly ◽  
Seismic Investigation ◽  
Regular Increase ◽  
Mohorovičić Discontinuity ◽  
Epicentral Region

Abstract Travel times are given as obtained from seismograms of the Witwatersrand earth tremors at distances up to 500 km. Five stations of several types were operated, which were moved as required. One method used continuous recording for a few hours daily; another used a triggering technique operated by radio from Johannesburg, where a network of six stations permitted the focus of each tremor to be located in time and place. Readings from the 200 seismograms obtained give velocities V1 = 6.09 km/sec. and Vn = 8.27 km/sec. for the P1 and Pn phases, and v1 = 3.68 km/sec., vn = 4.83 km/sec., for the corresponding S phases. Simply interpreted, these lead to a depth of 36 km. to the Mohorovičić discontinuity, including 5 km. of sediments confined to the epicentral region. There is evidence of a phase corresponding to an intermediate layer (the inclusion of which brings the total depth to 39 km.), but the data can also be interpreted to imply a regular increase of velocity with depth in the upper layer, as the presence of a local anomaly.

Particulate matter and particulate-bound mercury in a heavily polluted site related to ancient mining and metallurgy: a proposal for dry deposition modeling based on micrometeorological conditions

2018 ◽  
Vol 25 (35) ◽  
pp. 35312-35321 ◽  
Author(s):  
José Mª Esbrí ◽  
Celia Izquierdo ◽  
Alba Martínez-Coronado ◽  
Iva Miteva ◽  
Pablo L. Higueras
Keyword(s):  
Particulate Matter ◽  
Dry Deposition ◽  
Polluted Site ◽  
Deposition Modeling ◽  
Micrometeorological Conditions

A Technique for Continuous Recording of Subcutaneous Temperatures of Wild Mice

1951 ◽  
Vol 32 (1) ◽  
pp. 122-123 ◽  
Author(s):  
J. A. Sealander
Keyword(s):  
Continuous Recording ◽  
Wild Mice
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