scholarly journals Effects of bending portions of the air column on the acoustical resonances of a wind instrument

2012 ◽  
Vol 131 (5) ◽  
pp. 4164-4172 ◽  
Author(s):  
Simon Félix ◽  
Jean-Pierre Dalmont ◽  
C. J. Nederveen
Keyword(s):  
2008 ◽  
Vol 123 (5) ◽  
pp. 3447-3447
Author(s):  
Simon Félix ◽  
Cornelis J. Nederveen ◽  
Jean‐Pierre Dalmont ◽  
Joël Gilbert

2019 ◽  
Vol 105 (6) ◽  
pp. 899-903
Author(s):  
Timo Grothe ◽  
Sebastià V. Amengual Garí

A method is proposed here to synthesize the acoustic response of a room to a musical reed wind instrument with tone holes played by a musician. The procedure uses convolution of a) two measured pulse responses and b) the mouthpiece pressure during playing. The novelty of the approach is to include the sound radiation directivity of the source in the impulse response measurement of the room by using the wind instrument's air column as an exciter. At the reed input end of the air column pressure pulses at typical peak pressures of several kilopascals are generated using a compressor and a solenoid valve, which provides a high SNR even at distant measurement positions. For auralization purpose, the source signal measurement is done very close to the sound generation locus, i.e. inside the mouthpiece. Because this measurement is largely insensitive to room acoustics, the proposed method can be considered a very convenient alternative to music recordings in anechoic conditions. As a proof of concept we report here experimental results for the case of a bassoon. The method can be extended to auralizations of reed and lip-reed musical instruments in virtual acoustic scenes, and sheds light on the importance of the reflective and radiative properties of the air column for the sound coloration.


2021 ◽  
Vol 7 (7) ◽  
pp. eabe9510
Author(s):  
C. Fritz ◽  
G. Tosello ◽  
G. Fleury ◽  
E. Kasarhérou ◽  
Ph. Walter ◽  
...  

Anthropologists and ethnomusicologists assert that there is no society without song, and more specifically, there is no ritual or celebration without accompanying sound. The production of sounds in social contexts is very ancient. Here, we report on the study of a seashell from the decorated cave of Marsoulas and demonstrate that the Magdalenian occupants of this site transformed this shell into a wind instrument. It is one of the very rare examples, if not the only one for the Paleolithic period, of a musical instrument fashioned from a large shell, and the first conch shell of this use thus far discovered. We already know that prehistoric people transformed many shells into portable ornaments and that they thus attributed substantial corporal symbolism to them. This seashell horn, with its unique sonority, both deep and strong with an enduring reverberation, sheds light on a musical dimension until now unknown in the context of Upper Paleolithic societies.


2016 ◽  
Vol 29 (22) ◽  
pp. 8249-8267 ◽  
Author(s):  
Jian Shi ◽  
Weihong Qian

Abstract Using the daily mean anomalies of atmospheric variables from the NCEP Reanalysis-1 (NCEP R1), this study reveals the connection between anomalous zonal activities of the South Asian high (SAH) and Eurasian climate anomalies in boreal summer. An analysis of variance identifies two major domains with larger geopotential height variability located in the eastern and western flanks of the SAH at around 100 and 150 hPa, respectively. For both eastern and western domains, extreme events are selected during 1981–2014 when normalized height anomalies are greater than 1.0 (less than −1.0) standard deviation for at least 10 consecutive days. Based on these events, four SAH modes that include strong and weak Tibetan modes (STM and WTM, respectively) and strong and weak Iranian modes (SIM and WIM, respectively) are defined to depict the zonal SAH features. The positive composite in the eastern (western) domain indicates the STM (SIM) manifests a robust wavelike pattern with an anomalous low at 150 hPa, and surface cold and wet anomalies over Mongolia and northern China (Kazakhstan and western Siberia) are surrounded by three anomalous highs at 150 hPa and surface warm and dry anomalies over Eurasia. Opposite distributions are also evident in the negative composites of the two domains (WTM and WIM). The surface air temperature anomalies are the downward extension of an anomalous air column aloft while the precipitation anomalies are directly associated with the height anomalies above the air column.


1987 ◽  
Vol 9 (3) ◽  
pp. 216-223 ◽  
Author(s):  
S. Fuhrimann ◽  
A. Schupbach ◽  
U. Thuer ◽  
B. Ingervall
Keyword(s):  

1998 ◽  
Vol 51 ◽  
pp. 170 ◽  
Author(s):  
Richard Maunder
Keyword(s):  

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