Improved voice activity detection algorithm using wavelet and support vector machine

This paper proposes an improved voice activity detection (VAD) algorithm using wavelet and support vector machine (SVM) for European Telecommunication Standards Institution (ETS1) adaptive multi-rate (AMR) narrow-band (NB) and wide-band (WB) speech codecs. First, based on the wavelet transform, the original IIR filter bank and pitch/tone detector are implemented, respectively, via the wavelet filter bank and the wavelet-based pitch/tone detection algorithm. The wavelet filter bank can divide input speech signal into several frequency bands so that the signal power level at each sub-band can be calculated. In addition, the background noise level can be estimated in each sub-band by using the wavelet de-noising method. The wavelet filter bank is also derived to detect correlated complex signals like music. Then the proposed algorithm can apply SVM to train an optimized non-linear VAD decision rule involving the sub-band power, noise level, pitch period, tone flag, and complex signals warning flag of input speech signals. By the use of the trained SVM, the proposed VAD algorithm can produce more accurate detection results. Various experimental results carried out from the Aurora speech database with different noise conditions show that the proposed algorithm gives considerable VAD performances superior to the AMR-NB VAD Options 1 and 2, and AMR-WB VAD. (C) 2009 Elsevier Ltd. All rights reserved.

Antibody-mediated rejection (AMR) after pancreas and pancreas-kidney transplantation

P>Antibody-mediated rejection (AMR) requires specific diagnostic tools and treatment and is associated with lower graft survival. We prospectively screened C4d in pancreas (n = 35, in 27 patients) and kidney (n = 33, in 21 patients) for cause biopsies. Serum amylase and lipase, amylasuria, fasting blood glucose (FBG) and 2-h capillary glucose (CG) were also analysed. We found that 27.3% of kidney biopsies and 43% of pancreatic biopsies showed C4d staining (66.7% and 53.3% diffuse in peritubular and interacinar capillaries respectively). Isolated exocrine dysfunction was the main indication for pancreas biopsy (54.3%) and was followed by both exocrine and endocrine dysfunctions (37.1%) and isolated endocrine dysfunction (8.6%). Laboratorial parameters were comparable between T-cell mediated rejection and AMR: amylase 151.5 vs. 149 U/l (P = 0.075), lipase 1120 vs. 1288.5 U/l (P = 0.83), amylasuria variation 46.5 vs. 61% (P = 0.97), FBG 69 vs. 97 mg/dl (P = 0.20) and 2-h CG maximum 149.5 vs. 197.5 mg/dl (P = 0.49) respectively. Amylasuria values after treatment correlated with pancreas allograft loss (P = 0.015). These data suggest that C4d staining should be routinely investigated when pancreas allograft dysfunction is present because of its high detection rate in cases of rejection.

Protocolo de comunicación para AMR

Aquest projecte tracta d'aportar una idea al futur dels comptadors automàtics, on tant el usuaris, com les empreses, tindran un control continu sobre les dades. A més a més s’han buscar sistemes i protocols que realitzin una bona comunicació entre els comptadors automàtics, en aquest punt on entra la tecnologia W-Mbus. Aquesta tecnologia juntament amb els microcontroladors de baix consum, proporcionats per Texas Instruments, són la millor combinació per aconseguir el nostre objectiu.

Avoimen AMR-palvelualustan tiedonsiirtomenetelmien selvitys ja analyysi

Sähköenergiamittareiden etälukuun (AMR) siirtyminen on kasvanut Suomessa, kuten muissakin Euroopan maissa viime vuosina merkittävästi. Tavoitteena on, että vuonna 2014 80 % kaikista Suomen sähköenergiamittareista olisi etäluettavia ja rekisteröisivät tunnittaiset kulutustiedot. AMR-tekniikan avulla voidaan toteuttaa myös muita palveluja kulutustietojen rekisteröinnin lisäksi. AMR-mittareiden etäluenta ja niiden kautta siirrettävät signaalit vaativat mittareilta tiedonsiirtotapoja. Työssä tarkastellaan TeliaSoneran AMR-palvelualustan ominaisuuksia ja arkkitehtuuria. Selvitetään AMR-mittareiden toiminnallisia vaatimuksia ja mahdollisia tiedonsiirtotapoja mittareiden ja etäluentajärjestelmän välillä. Arvioidaan näiden selvitysten perusteella ja myös kustannusten kannalta eri tiedonsiirtomenetelmien soveltuvuutta eri ympäristöihin. Lisäksi suoritetaan arviointi ja käytännön laboratoriotestauksia valitulle sähköverkkoa tiedonsiirrossa hyödyntävälle AMR-mittarille. Tavoitteena on selvittää ja analysoida vertailtavan mittarin yhteensopivuutta TeliaSoneran päätelaitteiden ja AMR-palvelualustan kanssa. Analysoidaan näiden tarkasteltavien mittareiden ominaisuuksia ja elinkaarta. Laboratoriotesteillä selvitetään myös tarkasteltavien sähköverkkotiedonsiirto AMRmittareiden häiriösietoisuutta verkossa esiintyviä häiriöitä vastaan. Näiden pohjalta tehdään johtopäätökset ja suositukset.

JR WB ba

Brown sediment with clasts ranging from small to large in size. Clast shape ranges from angular to sub-rounded. Rotation structures are common in this sample, especially around larger clasts. Lineations and grain crushing is also present within this sample. A few comet structures can also be seen.

J.R WB-3a

Brown sediment with two main domains; a coarse grained domain and a fine grained domain. Clast size in the fine grained domain is mainly small. The coarser domain contains clasts ranging from small to large in size. The clast shape ranges from angular to rounded. Necking structures are commonly seen in the coarser domain. This domain also contains many rotation structures and lineations. The fine grained domain exhibits multiple water escape pathways, along with lineations. There are also minor amounts of grain crushing present within this sample.

J.R WB-6c

Brown sediment with clasts ranging from small to large in size. Grain shape ranges from angular to rounded. Lineations are abundant within this sample. Rotation structures can also be seen. Necking structures, comet structures, and grain crushing can also be seen in minor amounts.

J.R WB-7a

Brown sediment with clasts ranging from small to large. Grain shape ranges from angular to rounded. Rotation structures and necking structures are common throughout this sample. Lineations can also be seen throughout the sample, along with minor amounts of grain crushing and comet structures.

J.R. WB-2

Dark brown sediment with clasts ranging from small to large. Clast shape ranges from angular to rounded. Comet structures and lineations can be commonly seen throughout the sample. There are minor amounts of rotation structures also present. The sample contains clasts that are generally well dispersed.

WB-3b

Dark brown sediment with well dispersed clasts. The clasts range from small to large in size and sub-angular to sub-rounded in shape. The sample is abundant in rotation structures and lineations. It also contains comet structures and minor amounts of grain stacking.

WB-4

Brown sediment with clasts ranging from small to large in size. Clast shape ranges from sub-angular to sub-rounded. Rotation structures are abundant in this sample. They are seen around small and large clasts. A few necking structures can also be seen. These typically occur between larger aggregates. Lineations, comet structures, and grain crushing can also be seen in minor amounts.

WB-6a

Brown sediment with clasts ranging from small to large in size. Clast shape ranges from angular to sub-rounded. Necking structures are abundant within this sample, mainly between larger aggregates. Some rotation structures and lineations can also be seen. Comet structure and grain stacking can be seen in minor amounts.

WB-6b

Dark brown sediment with clasts ranging from small to large in size. Grain shape ranges from sub-angular to rounded. Rotation structures are common throughout the sample. Some necking structures are also present between large and medium sized aggregates. Lineations and grain stacks are also present in minor amounts.

WB-7b

Dark brown sediment with clasts ranging from small to large in size. The grains range from sub-angular to sub-rounded in shape. Rotation structures and necking structures can commonly be seen throughout. Lineations and comet structures can also be seen throughout the sample. Grain crushing can be seen in minor amounts in several areas.

WB-I

Dark brown sediment with two domains. One domain is fine grained, while the other is coarser grained. Clasts range from small to large, and sub-angular to sub-rounded in shape. The coarser domain contains lineations, comet structures and minor amounts of rotation structures. The fine grained domain is abundant with water escape structures. This sample also contains a few different areas of clay rich sediment.