Characterizing dusky dolphin sounds from Argentina and New Zealand

Dusky dolphin (Lagenorhynchus obscurus) acoustic sounds were characterized by analyzing narrowband recordings [0-16 kHz in New Zealand (NZ) and 0-24 kHz in Argentina], and sounds in broadband recordings (0-200 kHz) were compared to their counterparts in down-sampled narrowband recordings (0-16 kHz). The most robust similarity between sounds present in broadband recordings and their counterparts in the down-sampled narrowband recordings was inter-click interval (ICI); ICI was therefore primarily used to characterize click sounds in narrowband recordings. In NZ and Argentina, distribution of ICIs was a continuum, although the distribution of ICIs in NZ had a somewhat bimodal tendency. In NZ, sounds that had smaller mean ICIs were more likely to have constant ICIs, and less likely to have increasing or decreasing ICIs. Similar to some other delphinids, dusky dolphins may use single, short duration sounds that have a constant ICI and closely spaced clicks for communication. No whistles were documented at either study site. Temporally structured sequences of burst pulses (i.e., sounds with ICI < about 10 ms) also occurred at both study sites, and these sequences contained 2-14 burst pulses that appeared closely matched aurally and in spectrograms and waveforms.     

Polarised bidirectional reflectance factor measurements from soil, stones, and snow

The bidirectional reflectance factor and degree of linear polarisation of selected snow, soil, and gravel types have been measured using Finnish geodetic institute field goniospectropolariphotometer (FIGIFIGO). It was observed that with all measured samples the degree of linear polarisation is weakest 0–30 backwards from nadir, turning 1–5% negative in the backward direction, and growing larger (5–50%) in the forward and Brewster directions. Polarisation was found to be inversely but non-linearly proportional to reflectance. In addition, a wavelength-dependent trend was found to exist in some data, but in general, the wavelength dependence was smooth. Dry old snow polarises clearly more than melting snow or new snow. White gravel polarises somewhat similarly to snow in visible region, and black gravel resembles snow in infrared.The authors conclude that polarisation observations may be useful in land surface remote sensing, but that only far-forward angles (60–70) contain a strong enough signal for easy interpretation. The polarisation spectrum brings little additional information to reflection spectrum, but in conditions where the reflectance spectrum cannot be accurately normalised or incident irradiation is not known, polarisation spectrum could still be usable. The directional signal is strong and may yield refractive index or microstructure, and must be understood in any application. Polarisation near nadir is low for all known samples, and can thus be safely ignored with most non-polarised imaging applications. However, for accurate atmospheric polarimetry, e.g. by polarisation and directionality of the earth's reflectances (POLDER) or aerosol polarimetry sensor (APS) sensors, it is recommended to take into account land surface polarisation.     

Aspects of the acoustical design and properties of Christchurch Town Hall,New Zealand

The Christchurch Town Hall (2650 seats) is the major hall in a complex which includes a 986 seat theatre. It was opened on 30 September 1972 and was designed primarily as a choral symphony hall. Reverberation time (125 Hz to 2 kHz) in excess of 2·2 seconds with the hall full is provided by a volume of 20 500 m³ and reflective surfaces. The basic design aim, provision of relatively strong early lateral reflections, is achieved by large interior oblique reflectors which hang free from the boundaries of the reverberant volume. The resulting early lateral energy and long R.T. gives the hall a combination of reverberance, envelopment and clarity. The paper gives an account of design aims and studies including a ray tracing computer program with an interactive graphics output. Measurements of T₆₀, T₁₅ and integrated early energy have been carried out in the hall. Echograms and other measured data are presented. Clarity has been measured by a speech intelligibility test with the Hall empty except for 40 participants. With T₆₀ at 500 Hz 2·7 seconds, the intelligibility was better than the Peutz criterion for public address systems.     

高精度直流恒流源的设计与制作

本文介绍了一种高精度直流恒流源。这种电源简单易做，工作稳定。     

New nondestructive tests,from frames

The usefulness (Lubkin, 1976; Lubkin and Lubkin, 1979) ofB-plexes, an extension of Dirac's familiar observable (Dirac, 1947), is illustrated in a computation of all nondestructive tests over a system of finite ket-space dimensionn. These are tests whoseB outcomes are proportional to corresponding pure final states. The unitary motions of the system and aB-dimensional register, which effect such tests, depend very simply onn vectors from a frame inB-space. CaseB>n is not empty, and so presents nondestructive testing with nonorthogonal final states. The step where reduction of the wave packet happens, equivalently, computation of an Everett relative state, is given in an Appendix.     

Structure of 14C from 12C(t,p)

The reaction ¹²C(t, p)¹⁴C has been investigated with an 18 MeV triton beam. Twenty energy levels of ¹⁴C were identified up to 13 MeV excitation. Angular distributions were measured and compared with DWBA calculations. A previously unreported 0⁺ level at 9.75 MeV was observed; it undoubtedly corresponds to the second predominantly sd shell 0⁺ state in ¹⁴C. Additional spin and parity assignments have been made in the present work: 9.81 MeV, (1^?); 10.43 MeV, 2⁺; 10.50 MeV, (3^?); 10.74 MeV, 4⁺; 11.40 MeV, 1^?; 11.67 MeV, (1^?); 11.73 MeV, (5^?); 12.58 MeV, (2⁺, 3^?); 12.87 MeV. 2⁺, 3^?; and 12.96 MeV, (1^?); none of which had a definite spin and parity assignment previously. Our results confirm the previous information on the level structure of ¹⁴C below 8.5 MeV. The cross section for the unnatural parity state at 7.34 MeV, J^π = 2^?, is well reproduced by a two-step reaction calculation. The results are compared with the predictions of a weak coupling model.