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The question is what are the final goals of doing spectral analysis and what can we infer from that?
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Frequency spectrum of seismograms contain important information and depend on properties of the source (initiation), ray pathes (rock properties) and properties of receiver/recording equipment. If we know or can specify some of them we can deconvolve the seismogram and use spectrum to estimate the unknown parameters.
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I intend to use 4 half-degree aeromagnetic sheets for geothermal analysis with the intention of a 10' by 10' block size. But while I was going through some materials as references and citations, I got to realize the window size has to be large enough to capture the depth of the magnetic source.
I anticipate favourable answers and replies.
Thank you.
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Dear Isaiah Adelere,
I understand that your question does not have a unique answer, and it is made in geographical units ("...I intend to use 4 half-degree aeromagnetic sheets for geothermal analysis with the intention of a 10' by 10' block size...."). I will try to help with the following explanation:
First of all, you must put in geological/structural/tectonic context, it means: if your scenario is related to a relatively high heat flow regime, the window size should be small enough to estimate the Curie point depth (CPD) because it is expected to be shallow. In contrast, if your geological scenario is considered a low heat flow, it should be large enough to estimate the deeper CPDs. It means several window sizes you must test, and the appropriate length must be selected based on the criteria of the minimal block size that does not cut off the spectral peak (Ravat et al., 2007).
On the other hand: if you have land, airborne, or satellite data, the filtering effect of anomalies could be critical, also the spectral answers. Therefore, the question is: Which is your data source for your research? Satellite magnetic data complement the existing local and regional data sets by providing a globally unified data set. It means: the local structures below the minimum wavelength content cannot be resolved in such a data set, therefore: you must choose the window size for FFT and CDPs estimation according to or in the function of your dataset.
The methodology that I recommend using to estimate Curie point depth is founded on the 2-D radial average power spectral (RAPS) analysis of magnetic anomaly data described basically by three foundational works:
  • 1) Spector and Grant (1970), where estimated the depth to the top of magnetized rectangular prisms (Zt) from the slope of the log power spectrum.
  • 2) Bhattacharyya and Leu (1975a, b, 1977) calculated the depth of the centroid of the magnetic source bodies (Z0).
  • 3) Okubo et al. (1985) developed a method to estimate the bottom depth of the magnetic bodies (Zb) using the spectral analysis method of Spector and Grant (1970).
Mathematically, the Fourier transform of a space domain function f(x,y) is measured in radians per meter if x and y are in given meters. These are related to spatial "frequencies" fx and fy, in cycles per meter. All spectral analysis must be in distance units, such as meters, not in geographical coordinates such as latitude and longitude. FFT will take the 2-D forward Fast Fourier Transform and perform one or more mathematical operations in the frequency domain before transforming back to the space domain. An option is provided to scale the data before writing the new values to an output file. The horizontal dimensions of the grid are assumed to be in meters. For other grids geographical grids were you want to convert degrees into meters.
The input dataset of a magnetic anomaly - the emphasis for land research - must reduce the influence:
  • 1) Boundary conditions and edge effects;
  • 2) Avoid high-frequency noise caused by tiny structures near the ground after lowpass filtering.
  • 3) The reduction to pole (RTP, Baranov, 1957) must be applied to the magnetic anomalies to obtain anomaly values induced by the inclination of 90º and the declination of 0º. In theory, appropriate only when all bodies/sources in your ZOI are magnetized parallel to the geomagnetic field and at the same time it has a vertical dip.
The depth estimation from your RAPS advises you that the optimal square window dimension is about 10 times the estimated depth (Chiozzi et al., 2005). Thus, you should divide your work area/zone of interest (in km/m units) into square subareas of such as for example 300 km x 300 km to say you an accurate value, each of them overlapping with respect to each other in a step increment, for example, 100 km, and then applying the 2-D FFT RAPS method individually to get Zo and Zt. The computation requires an extensive dataset for estimating Curie point depth.
Best regards, Mario E. Sigismondi
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I am looking at local field potentials and brain oscillations in vitro and am wondering if the power spectral analysis can be performed in clampfit. Most manuscripts report using a custom script in Matlab concurrent with pClamp softwares. I am curious if all analysis can be performed in Clampfit.
Data need the transformation first. I do not know if this can be done.
Any help would be greatly appreciated.
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Yeah, I have seen a majority of papers use MatLab after data acquisition. Thank you for response. I am less familiar with the MatLab coding language and software use. I guess its the next thing I need to learn!
Thanks again, Dr. Bjorkland
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I would want to know the fundamental difference between eigenvalues and singular values when applied to spectral analysis of graphs' adjacency and laplacian. As far as I know the SVDs can be worked on nonsquared matrices but adjacency and laplacians are squared matrices and they would be symmetric if the graph is undirected.
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please just check wiki:
singular value decomposition ... generalizes the eigen decomposition of a square normal matrix ... to any m-by-n matrix
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We will be very grateful for a discussion, experience sharing, possible experimental challenges for the accurate and reliable photoluminescence (PL) investigation of 2D TMDC layers/films (WSe2) using Spectrofluorometer with a monochromatic light source (Xe arc lamp).
We have performed PL spectral analysis of various WSe2 films (mono- and multilayered) on different substrates (c-cut sapphire, fused silica, SiO2, Si).
PL properties of WSe2 (and other semiconducting TMDC) are extensively investigated with a strong thickness dependence and usually broad peaks structure. The majority of the PL studies are based on a laser source configuration, while the PL analysis of TMDC thin films using Spectrofluorometer are very rare.
However, our acquired spectrum (for all studied thin film samples) is untypical and consists of single very narrow peak at 754nm(1.64eV) with linewidth ~ 10meV at λexc = 500nm.
The samples are produced by Chemical Vapour Deposition and Thermal Assisted Conversion.
Thank you!
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Hi,
Firstly the noise which is coming in your sample is due to scattering (lamp phenomena). Secondly sometimes lamp intensity is not so high that can excite and gives you emission. Is this peak matches one with the literature or laser based pl system.
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I'm doing spectral analysis of a signal. I compute psd.
In order to get better results and good accuracy, i use windowing.
I was wondering how to choose number of blocks in the window.
Let's assume that i'm dealing with 15000 data points, and i choose hamming window.
in the script, i write:
ham=hamming(number_of_blocks); %number_of_blocks=100? 1000?
Thank you in advance
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Thank u
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Spector and Grant 1970 have shown that spectral analysis can be used for depth estimations of causative anomalies located at different depths. They have used aeromagnetic data. Is it valid the same formula for gravity anomalies or does it need a correction? I have searched many articles in which at least 50 % were implemented wrong. Some of the articles used half of the slopes as the depth some used 1/4pi of the slope. It is actually quite confusing how people use and misuse this method. The decay of gravity anomaly is less than magnetic so I am wondering if gravity needs any correction or derivative before using the spectral analysis for finding depths.
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Good evening Aziz,
As a start point, you may use Hinze et al., 2013, Chapter 7; Gravity anomaly interpretation; pages 192 and193 and the references therein (I have attached it in a message).
I hope this would helpful,
Best regards,
Hayder
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Different cascaded fiber structures such as single-multi-single (SMS) mode, multi-single-multi (MSM) etc. have unique spectral features due to the multimode interference (MMI) phenomena. The transmission spectrum depends on the sensing fiber length i.e., SMF and MMF for MSM and SMS, respectively at the time of fabrication (ignoring the effect of external perturbations).
How does the group dispersion phenomenon affect these spectral features?
The spectrum of one of such cascaded fiber structures (here MSM) has been attached for the reference that occurs due to the MMI phenomena.
#fiber #SMS #MSM #Groupdispersion #opticalfiber
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Thank you so much Jawher Makhlouf for sharing the article. I will go through it.
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We had a question in this article. How did they calculate a single band value representing all 64 electrodes to compare between-subject groups? Usually, a specific band (i.e., alpha) should have 64 pieces of data towards corresponding 64 electrodes.
The table shows that each participant have a single rest data for one specific band, and then research use independent t-test to compare between two groups.
Can any experts help us to understand this?
Reference:
Ding, Y., Cao, Y., Qu, Q., & Duffy, V. G. (2020). An exploratory study using electroencephalography (EEG) to measure the smartphone user experience in the short term. International Journal of Human–Computer Interaction, 36(11), 1008-1021.
Zhepeng
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The authors write this: "A digital FFT (fast fourier transform) based power spectrum analysis (Welch technique, Hamming windowing function) was used to compute PSD average value of EEG with NFFT = 1024, window = 512 and 50% overlapping window. An average absolute power value of each electrode for each frequency band was calculated. An average of the pre-experimental absolute power was used to determine the individual power during rest. The power of the rest period was set as the baseline. From this reference power value, individual power changes during smartphone use were determined as the relative stimulus-related change. The relative power of each band was calculated for statistics (e.g. α/(sum of the powers from all five bands))."
From my experience and from what I can see is written, this means that they calculated the average power for all electrodes in a given band. This simplifies the analysis but looses a lot of information on location, for example, of any differences detected.
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Our research team met one question on calculating EEG relative power and absolute power at this stage.
When we integrated all negative and positive amplitude/power data in five EEG bands (delta, theta, alpha, beta, gamma), a few relative power results became huge (i.e., 440%(44.44) or even over 1000%). We thought these values were abnormal results. The reason is that the integration result of five EEG bands with negative and positive power values could be 1 or 2 as the denominator, but the numerator could be very large for the integration of one specific band(i.e., delta). The relative power calculation is (sum of spectral power in the band)/(sum of spectral in all bands)
The attached image showed some negative and positive spectral power values.
Therefore, we would like to ask whether we need first to transfer negative value to absolute value to consider relative power or absolute power. Normally, the relative power should be around 0-100%.
Can experts help us? Could experts please share some references with us?
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First it is better to calculate the density of the power spectrum (PSD) of the signals and continue the calculations based on it. The value of the PSD is usually not negative. Delta values are usually higher than other frequency bands. Consider starting the Delta wave frequency range from 0.1 or 0.01 Hz and not from zero. If you have collected signals from several samples and the average PSD of the frequency bands in the different samples is very different, you must first normalize the PSD values calculated from each sample in each frequency band. To do this, first calculate the PSD of the data collected from each sample. Then calculate its standard deviation in each frequency band. Divide the mean values for each frequency band by its standard deviation. In this way the data is normalized. You can now use these values to calculate relative power.
Best regards
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The general consensus about the brain and various neuroimaging studies suggest that brain states indicate variable entropy levels for different conditions. On the other hand, entropy is an increasing phenomenon in nature from the thermodynamical point of view and biological systems contradict this law for various reasons. This can be also thought of as the transformation of energy from one form to another. This situation makes me think about the possibility of the existence of distinct energy forms in the brain. Briefly, I would like to ask;
Could we find a representation for the different forms of energy rather than the classical power spectral approach? For example, useful energy, useless energy, reserved energy, and so on.
If you find my question ridiculous, please don't answer, I am just looking for some philosophical perspective on the nature of the brain.
Thanks in advance.
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Hi,
The mitochondrion in cells is a powerhouse of energy. There are some articles on the topics of your interest:
Jeffery KJ, Rovelli C. Transitions in Brain Evolution: Space, Time and Entropy. Trends Neurosci. 2020;43(7):467-474. doi:10.1016/j.tins.2020.04.008
Lynn CW, Cornblath EJ, Papadopoulos L, Bertolero MA, Bassett DS. Broken detailed balance and entropy production in the human brain. Proc Natl Acad Sci U S A. 2021;118(47):e2109889118. doi:10.1073/pnas.2109889118
Carhart-Harris RL. The entropic brain - revisited. Neuropharmacology. 2018;142:167-178. doi:10.1016/j.neuropharm.2018.03.010
Sen B, Chu SH, Parhi KK. Ranking Regions, Edges and Classifying Tasks in Functional Brain Graphs by Sub-Graph Entropy. Sci Rep. 2019;9(1):7628. Published 2019 May 20. doi:10.1038/s41598-019-44103-8
Tobore TO. On Energy Efficiency and the Brain's Resistance to Change: The Neurological Evolution of Dogmatism and Close-Mindedness. Psychol Rep. 2019;122(6):2406-2416. doi:10.1177/0033294118792670
Raichle ME, Gusnard DA. Appraising the brain's energy budget. Proc Natl Acad Sci U S A. 2002;99(16):10237-10239. doi:10.1073/pnas.172399499
Matafome P, Seiça R. The Role of Brain in Energy Balance. Adv Neurobiol. 2017;19:33-48. doi:10.1007/978-3-319-63260-5_2
Engl E, Attwell D. Non-signalling energy use in the brain. J Physiol. 2015;593(16):3417-3429. doi:10.1113/jphysiol.2014.282517
Kang J, Jeong SO, Pae C, Park HJ. Bayesian estimation of maximum entropy model for individualized energy landscape analysis of brain state dynamics. Hum Brain Mapp. 2021;42(11):3411-3428. doi:10.1002/hbm.25442
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Hello everyone! I'm doing a study based on comparing spectral indices from Sentinel-2/MSI and Landsat-8/OLI data. The Sentinel-2/MSI - Level-1C are provided on TOA reflectance data, and Level-2A on BOA reflectance data. However, Landsat-8/OLI data are provided only on BOA reflectance through Collection 2, Level 2. Considering that I have to convert the Landsat-8/OLI Collection 2, Level 1 data to TOA reflectance, do I need to do another type of pre-processing in all other data?
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You can use surface reflectance datasets for both, Sentinel and Landsat-8, which area already atmospherically corrected.
Google Earth Engine Snippet:
Sentinel image Snippet: ee.ImageCollection("COPERNICUS/S2_SR")
Lt 8 image Snippet:ee.ImageCollection("LANDSAT/LC08/C02/T1_L2")
In order to compare these two datasets using spectral indices, as a preprocessing step, you have to harmonize them. You can read more about this process in these articles.
A GEE tutorial that might help.
Good luck.
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Is there any automated peak finder program for mineral identification with Raman data ? 
Or any data set as peak library or spectral library in this field. 
I know some websites that have some data but I need a program software or a good data set as library for mineral identification.
Thanks every body.
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The best software and database is "Know-it-all" but it is not free.
Here the collection of resources wich could be used to analyse Raman spectrs it include mention early RRUFF an many more: https://www.researchgate.net/post/Free-Database-with-Raman-spectra
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We can measure exchangeable K, Ca using flame photometer. Is it possible to analyse these ion using spectral analysis
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You can measure the exchangeable cations using Ammonium Molebdate solution under spectroscopy.
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Hello dear Researchers, I need guidance related to derampdemod. working with single SLC_IW data, after applying derampdemod signal encountered with stripes. https://sentinels.copernicus.eu/documents/247904/1653442/Sentinel-1-TOPS-SLC_Deramping.pdf/b041f20f-e820-46b7-a3ed-af36b8eb7fa0?t=1533744826000 1 Anyone who worked with this process is given in the above link, actually, I need to produce figure.2. spectrum after derampdemod. I have attached one intensity image and after derampdemod I encountered stripes. Looking forward to your advice.
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Roland Akiki Muhammad Amjad Iqbal Hi Roland and Amjad,
Would you please let me know how can I apply de-ramping and re-ramping on S1 data? I have access to GAMMA and ESA SNAP, but couldn't find any module to re-ramp the data—Is there any open-source or freely available matlab/python code for these two processes?
Many thanks,
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I am looking for a software which can take a txt file of a spectra obtained from an OES device, detect the peaks, and qualify the element/atom that is associated to the peak with some probability. Does anyone have experience with any such software?
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With free optical spectroscopy software http://Spectragryph.com, you can load your txt file(s), activate "Peak labels", choose "LIBS" label type and have peak labels with element names shown automatically. With the "Peaks & FHWM" function, you can create peaks lists with peak positions and element names, also for a batch of spectra at once.
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I am trying to compare a time series data by these two methods: Holo-Hilbert spectral analysis and Hilbert-Huang transformation.
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Repeat the attached screenshot search and follow the details. Best wishes David Booth
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I regularly doing ATR-FTIR analysis from several mineral oil and surfactant, lately i discover a strange and unknown peak appear (1000-1300 cm-1) which is not belong to the material absorbance (i'm pretty sure because I have previous measured spectra from the same sample).
In the attachment, I put Fig 1 as the comparison of previous measurement and the current spectra.
I did a background scan and follow with scanning empty sample, and I can get straight line without any obvious noises. (fig 2)
Is there anyone having the same issue or know what happen with the spectra result?
In the other hand, i found this file (Fig 3) appear in my storage folder which I don't know where its coming from.
Is there any relation between this file and the issue in my FTIR spectra?
Kindly advice, thanks!
nb: I use Perkin Elmer FTIR
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The logical thing is to think that the sample has changed (it has reacted, degraded, etc ...) Knowing what sample it is would help to see what may be the cause of this spectrum change ...
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I want to compare the experimental measurement of the spectrum at river confluence with the theoretical model. Can we apply von Karman spectral model for river flows, particularly at the shear layer? Please suggest other models, if any, with references.
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I am not familiar with Von Karman model use in Rivers, or even wind turbulence. River confluences can be very complex, and actually for rivers with floodplains, the confluence location may shift for flows below bankfull, and above bankfull. And braided streams might even have multiple confluences shifting with flow, and channel shifting due to excessive sediment, woody or organic debris accumulations, etc. Whether HEC RAS or Rivermorph models might be helpful to your questions, I don’t know. My advice if you want to collect data would be to purchase or find assistance from water scientist, agency or university that has a Doppler flow meter, that is able to collect flow depth, velocity details as it is pulled across the specific cross sections of interest. In relatively clear rivers, Green LiDAR might also be helpful in remotely collecting some channel morphology and associated data. During drought or dry periods, LiDAR might also be helpful in revealing some exposed channel complexities, although the LiDAR pulses are absorbed by water.
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Hi I'm looking for some mineral and rock spectra repositories to use in the interpretation of remote sensing images and spectral mapping for mineral prospecting and research.
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Typical positive congo red spectral assay for binding to amyloids would be an observation of spectral shift from 498nm (CR only) to 540nm (in presence of amyloids). However I've tried the both the spectral assay and the birefringence assay (http://www.assay-protocol.com/biochemistry/protein-fibrils/the-congo-red-birefringence-assay) with an amyloid sequence AB(27-32) peptide that forms amyloid fibers, the spectra I've got does not shift to 540nm, there was only an increase in absorbance at 498nm. Under polarized light microscopy the fibers do appear to be apple green and birefringent after staining with Congo Red though. What is wrong? Or is it normal to get an increase in intensity of the spectra instead of spectral shift?
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Also had such problem. I use Congo Red for studying amyloids in a biofilm matrix. With comparable visualization of the staining density, I found that 540 nm works best for me, no more, no less.
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I have downloaded SDSS specra data of the dwarf galaxies for my study. I am studying strongest emission lines. I am bit confused, whether we need to perform a baseline correction beofore the measurement or not. Need your help. Thanks.
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Yes, in order to measure the line flux (and subsequently - luminosity) you need to subtract the continuum. There is a simple explanation for this. Imagine that your galaxy has 10 times more stars but the same SFR. Then the continuum level will go up by a factor of 10, so if you don't subtract it you would measure SFR 10 times higher, which would be wrong.
By the way, check the SDSS catalogues - maybe your galaxy already has the H alpha flux measurement.
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I am interested to perform spectral analysis of a structure under random waves. could anyone suggest me a book or an example that starts from wave spectrum (such as
JONSWAP spectrum , P-M etc) to RAO. A complete example from formulation to numerical evaluation.
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Dear All!
Is there a software in which I will make NMR prediction of compounds in deuterated acetontrile, acetone or methanol ? In mestrenova I can make only predictions in chloroform, dmso or water.
Thank you so much for your help!
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Mrs/Miss Haraźna,
Do you know the reliability of these so called predictions of NMR spectra?
There is a plenty of software for prediction of mass spectra as well. However, a comparative analysis with experiment shows a dramatic lack of accuracy between theory and experiment.
Such software are very useful to only educational purpose. Because of, all important and really observed both NMR and mass spectrometric phenomena are unable to be accounted. Thus, the so-call predicted spectra produce very illustratively the fundamental basick knowledge.
An additional comment on: RG represent forum for exchange of knowledge at a highly specialized professional level. Very frequently, many participants are unable to distinguish between highly specialized technical information and low specialized information of general or popular character. The latter one is typical for the public press. Owing to the fact that the comments on RG are inaccessible to the mass reader or to the communities as whole, this means that RG does not represent forum for distribution of knowledge at a general public level.
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Is there any information about refraction indices and extinction coefficients for some types of Stainless Steel?
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Not sure if it has stainless steel, but a good reference to have saved nonetheless.
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I need information concerning the penetration and reflection capacity of ultraviolet and infrared radiation wavelengths on different most common materials.
Edit.
Can somebody recommend a book to learn about? I'm especially interested in spectrogroscopy with a city environment materials and albedo.
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First of all it depends to the material studied, and for me i guess that IR is more better then UV cause its wavelength is bigger than UV.
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In several discussions, I have often come across a question on the 'mathematical meaning of the various signal processing techniques' such as Fourier transform, short-term fourier transform, stockwell transform, wavelet transform, etc. - as to what is the real reason for choosing one technique over the other for certain applications.
Apparently, the ability of these techniques to overcome the shortcomings of each other in terms of time-frequency resolution, noise immunity, etc. is not the perfect answer.
I would like to know the opinion of experts in this field.
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Utkarsh Singh There is an esthetic reason in why a mathematical method is of interest in signal processing:
-a beautiful algorithm is well articulated, says what it does in few instructions, and does it in a stable and reliable manner
-this hints to the underlying algebra
With powerful and minimal computation, we go deep into algebra structures: group, rings, fields (see references on Evariste Galois as the inventor of "group" as we know it)
-Fourier transform is an interesting invention: it allows to decompose a signal into resonating modes (as for piano music: you produce a sound at frequency F, but also its harmonic NxF...). Naturally there is the aliasing question and the Nyquist theorem for reconstruction
There are many more time-frequency representations: Fourier, Laplace, discrete or continuous, cosine transform, wavelet transform, etc.
The interesting feature of discrete algorithms for those transforms is that you can implement a butterfly structure.
The key idea is to replace a very large number of multiplications (in brute force "non-esthetic" programming) by a smaller number of additions.
This idea worked for me for developing a codec system using underlying GF(n) properties.
See this patent:
The regularity in the processing and the efficiency of the representation go hand in hand.
Let me go back to a very basic mathematical method: the Gram-Schmidt decomposition: take a sequence of n vectors v(1),..., v(n), and the matrix of cross-products m(i,j)=<v((i),v(j)>. The Gram-Schmidt method diagonalises this matrix. It extracts eigenvalues, and eigen vectors. In frequency terms, it extracts modes (resonating modes present in the signal).
This algorithm highlights the efficiency side of the representation: it's projecting the signal onto something found "in itself", call it principal components if you want.
There are only two reasons for choosing a technique in engineering:
-(i) it addresses the problem completely
-(ii)it's economically implementable.
Both criteria are equally important and a good way to find these is to look for elegant, esthetic solutions (minimal and complete at the same time).
Does it help?
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Hi,
I am working on an echo removal project. So far, I have successfully identified the far-end signal of length 21 ms at a sampling rate of 48000Hz whose echo is present in my near-end signal of 21ms. I did it using Echo Detection and Delay Estimation using a Pattern Recognition Approach and Cepstral Correlation .
Now, I want to remove that far-end echoed signal from my near-end signal which contains(echoed signal of farend and voice).
Things I tried:
  1. Time-domain subtraction of PCM signals. i.e output[n] = near_end[n] - far_end[n]
  2. Spectral Subtraction technique Eliminate Signal A from Signal B. Even Ephraim-Malah
In both, I am not getting the expected result as for spectral subtraction I read that It works well when there is static noise or one signal is stationary. For non-stationary signals, it doesn't work well.
What are the other techniques to remove the echo in my scenario? Since I have identified the far-end chunk whose echo is present in the near end chunk, I just want to remove it from near end chunk.
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Isam Alkhalifawi Sir, these adaptive echo cancellation techniques don't help me in my scenario. My echo is non-stationary and the same sound is being produced with delay by multiple speakers, not just 1 speaker.
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I was reading "Time-Series Anomaly Detection Service at Microsoft" (https://arxiv.org/pdf/1906.03821.pdf) in these days, and I got some problems for the programming part.
The first picture shows the algorithm, the general idea is to perform the fast fourier transform for a time series sequence, calculate the spectral residual and perform inverse fast fourier transform at the end. When I checked the official code of this paper, before performing the inverse fast fourier transform, the transformed signal ('trans' in the code) was multiplied by the spectral residual and then divided by its amplitude (line 212 - 215 in the second picture) which is confused. If someone can explain about this part? Thanks.
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We are trying to map land cover classes on a watershed. We have selected training sites (during a field campaign in early 2017) and extracted their spectral profiles based on a Landsat 8 image acquired at the time of field surveying.
In order to assess the land cover changes, we wanted to map the same cover classes at a previous year. Since our training sites might not be relevant, we wanted to perform supervised classification using endmembers spectra instead of ROIs. When importing those spectra inside ENVI's Endmember Collection toolbox, it appears that only Spectral Angle Mapper and Spectral Information Divergence classifiers could be used. Common algorithms such as Maximum Likelihood or Mahalanobis distance fail, returning the following error message :
Problem: the selected algorithm requires that the collected endmember spectra all contain an associated covariance. ENVI is unable to continue because some of the endmembers collected to not have their covariance.
Could anyone help here ? Actually is our method relevant ? How can we possibly perform supervised classification using Maximum Likelihood/ Mahalanobis classifiers on some older satellite images ?
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Roland Yonaba Aline de Matos Valerio Roland questioned himself as to whether the method is relevant. It is not. Methods such as SVM or Mahalanobis distance or Random Forest rely on a data distribution, thus the covariance that is derived from the many pixels in a region of interest taken for training. With the endmembers, you have only one example of each endmember spectrum. SAM and other methods can work with the endmembers because they are just calculating a distance in spectral space between each image pixel spectrum and the endmember spectrum.
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I am working with the spectral irradiance on different planes. The readings are available on a global horizontal and plane of the array of 45 degrees. I have a PV module inclined vertically and I want to apply the transpositional model to calculate the spectral irradiance at a vertical plane. I am looking for a reliable model, which I haven't come across, unfortunately.
I believe, spectral albedo would be the deciding factor on these models, even more so compared to the broadband albedo. Can someone suggest any spectral irradiance transpositional models? That'd be a great help.
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Chris Gueymard Thanks for the suggestion. Yes, I have been thinking to use SMARTS. But I was also curious to know if there are any other transpositional models that transform the spectral irradiance from global horizontal to tilted plane.
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I have observed that there are usually a dip in the spectral ordinate (Sa/g) at short period (<0.1s) for the ground motions obtained using stochastic simulation (SMSIM). I have attached a figure highlighting this. The same can be observed for the spectra obtained using some GMPEs (which are developed using synthetic ground motions).
However, I have seen this dip to be absent in the median spectra (Sa/g) of horizontal component obtained using recorded ground motions or the spectra obtained using GMPEs (which are developed using recorded ground motions).
I believe this dip is due to spectral De-amplification for which is higher in medium/stiff soil site and covered in SMSIM. What is the reason that this dip is not observed in recorded data?
However, this may also lead to inconsistency in GMPEs for the same region generated using real ground motions and synthetic ground motions.
I am particularly new in this area and would really appreciate some answers.
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Hi Ravi
I would recommend to start checking the frequency band over which you perform the SMSIM simulation. This kind of short period trough could be due to high-pass filtering - or absence of HF computation - at frequencies around 5-20 Hz. Have a look at the Fourier spectra of your SMSIM acceleration time series and compare it with the expected typical shape (log-log scale).
Do you have similar troughs whatever the site conditions ? What is the "kappa" value you consider ?
Hoping it will help, all the best
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I want to plot the lower and upper confidence with the spectral density plot to find the significance of the peaks. Any help would be appreciated.
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It's how to to convert spectral radiance from W/cm^2/sr/nm to W/cm^2/sr/cm-1. Fisrt one is the radiance represented by wavelength and second one is represented by wavenumber.
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these two units do not have a linear scaling relationship. rather, this depends on wavelength. wavenumber ν [cm-1] relates to wavelength λ [nm] as v = 10^7/λ. when integrating the same radiances (in their appropriate units) over the same finite spectral interval (in either wavenumber or wavelength), the answer has to be the same. from the differential dv/dλ = -10^7/λ^2, it follows that dv = -10^7/λ^2 dλ, and therefore [W/cm^2/sr/cm^-1] = [W/cm^2/sr/nm] * 10^7 / λ^2.
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If it possibility to take Metal doped nano SnO2.  Please guide me for measurements
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Yes, we have synthesized the SnO2 nanoparticles by chemical co-precipitation method. we have made the FL life time measurement to study effect solvents and calcination temperature on life time of carriers of synthesized sample. Refer our article "Strctural and Optical properties of Zirconium Oxide nanopaticles : effect of calcination temperature " which we have published recently in Nano Express. We will publish articles on life measurement on SnO2 nanoparticles soon.
Best of luck.
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Spectra collected during chemo metric experiments like tit-ration stop flow reaction etc
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First of all what is the purpose of the programme? I mean, what is the subject?
If you study about Astronomy, I suggest iSpec analysis programme.
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I use Spectral Kurtosis and Kurtogram to study the turbulence of financial markets. I would like your advice concerning the intuition behind Spectral Kurtosis and Kurtogram.
- Financial Crisis
- Kurtogram
- Spectral Kurtosis
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I have made somce applications in finance. Could you help for comments and discussion on my results ?
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In estimating the texture distribution of asphalt mixtures, i have managed to use the discrete fourier transform on my idealized surface profile and obtained my spectral power density.
However the process of Transforming constant bandwidth spectral data to constant-percentage
bandwidth spectral data has proved challenging i would appreciate assistance in understanding and progressing from my current stage.
I have attached the excel sheet and an image of the formulas from ISO 13473-4
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the formula sheet
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I know there are free current satellites such as Landsat, sentinel and planet. but i want to know whats the new satellites which provide free images with high resolution.
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Try with ASGS website..
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According to the articles, we use fourier transform to compute power spetra density(psd) in spectral analysis ,
Sm = psd = lim {2|Ym|^2 /( N * delta) }, m=1,2,3,..., N / 2
psd is a function of frequency ( Fm = m / N),
In the logarithmic graph, Fm is expressed in terms of Sm.
Sm ~ Fm ^(- Beta) ---> log Sm ~ log Fm^(- Beta) ---> Beta (spectral exponent) = - log Sm / log Fm
the relation of spectral exponent with fractal dimension :
Beta = 5 - 2 D ----> D = (Beta - 5) / 2
for example : 0 < Beta < 1 ---> 0 < 5 - 2 D < 1--> 2 < D < 2.5
Answer range for fractal dimension(FD) : 2 < D < 2.5
I want to know what is the direct impact of the fractal dimension on the analysis of the Rossler system?
In other words, How can I connect this answer range(FD) to the analytical solution of Rossler system?
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Thanks for the files, I hope leads me to better understanding.
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Does anybody know a free online UV-Visible spectra database for inorganic salts, e.g. NaNO3, NaNO2, NH4Cl, K3PO4? 
I hope there are some databases for UV/Vis spectra where raw data could be downloaded. Like this, Fourier Transform Infrared (FTIR) Reference Spectra https://www3.epa.gov/ttn/emc/ftir/refnam.html 
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You can try spectroscopy Ninja. it is open source https://www.effemm2.de
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Hi i am a Medical Physics PhD student, im interested in Radiolysis and production of free radicals, i am very curious is to collect information is there any possibility to measure the free radicals, singlet oxygen in vivo and vitro. My idea is to measure the spectral changes.I would appreciate suggestions or possibilities if any.
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You can use some chemical probes such as APF (aminophenyl fluorescein) or SOSG (singlet oxygen sensor green). You measure probes' fluorescence before and at the end of the irradiation. Fluorescence enhancement will indicate ROS or signlet oxygen generation.
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Is there any standard procedure/sequence of tools to process the hyperspectral tabular data before PLSR regression modeling.
example of tools are 1) De-resolve 2) second derivative 3)normalize 4) de-trending 5)baseline etc.
Application is for field spectroradiometer data of soil and crop.
Or the sequence of tools differ for different datasets ?
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The pre-treatments you use will depend on the sample set: noise, level(s) of analyte, number of samples, ranges, etc. In many cases, it is a case of start small (Absorbance data) and add treatments, as needed. Just remember, every treatment can hide/generate peaks and will have an effect on sensitivity.
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Cavity modes are a consequence of constructive interference of EM waves in a particular region. It is common knowledge that the (frequency) linewidth of a cavity resonance is broadened by both homogeneous (energy loss/damping) and inhomogeneous (non-uniform environment) effects. The linewidth due to homogeneous damping is inversely proportional to the lifetime of the cavity mode. I believe that 'integral intensity' of the resonance uniquely defines how much energy is within the mode, and that the integral intensity and the linewidth in combination uniquely define the amplitude of the mode.
I am curious about resonances of destructive interference. They can also be characterized by a linewidth, integral intensity, and an amplitude. However, in this case, the resonance corresponds to the absence of EM modes at a particular frequency. What do linewidth, integral intensity, and amplitude indicate for a resonance of destructive interference? It should be pretty similar, because both cavity modes and destructive interference resonances are the consequence of interference, the only difference is whether the interference is constructive or destructive.
Maybe there are some texts of spectral analysis or characterization of resonances that could help clarify this?
Thanks!
-Ryan
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Dear Researcher,
Your question is interesting. Unfortunately I do not know the answer but I will follow your question and if you find something interesting, I attach it.
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I have send my extracts for GCMS analysis. The problem is I don't really know how to classify it. I am also not good in chemistry. I have read papers and researchers always group their components. Do I need to go through each compounds one by one and identify whether this one fall under what group? 
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I'm also struggling the interpretation of my GC-MS results. that's the problem of not a chemist.
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I want to get a time-frecuency spectogram using windowed burg and lomb-scargle method. As long as I know they calculate the psd for a segment of time. But for shot signal(less than 5 min of length). The recommended window sizes are bigger than the singal length so I get only a psd for the whole signal. So what window size should I use in order to get a 5 min time frequency spectogram for a 5 min signal.
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The window size of the STFT should be short enough to maintain the stationarity of the signal. If the frequency characteristics change in a window, you can set the window size shorter. Check the periodicity of signal in the time domain, and and determine the window size short enough to catch the periodicity.
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I am looking to make an Echinochrome A calibration curve for microplate visual spectral analysis of S. purpuratus coelomic fluid.
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Hi Jessica,
You may make an inquiry at Alfa Chemistry, they offer kinds of chemicals for research use.
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We want to show the surface changes to PET and PLA plastics (in pulverized form) as a proof of the UV treatment. From what I understand ATR is useful for spectral analysis of a solid, but I read that it cannot be used for "hard" polymers/powders. Are PET and PLA compatible with this method or is there something else I should look into?
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Neither of those polymers are too hard to obtain good ATR spectra. If you do the experiments carefully and run control samples you should be able to see the chemistry changes. There are a few things to keep in mind. A diamond ATR will allow you to apply a lot more pressure to the sample and using a high pressure clamp will help. Depending on the amount of treatment, you may need to be careful of the penetration depth. If the ATR element you use gets too deep a penetration, the bulk material may "wash out" the spectrum of the treatment. And if you are planning to compare to library spectra make sure you take into account (or correct for) the wavelength dependent depth of penetration. I would strongly suggest reading this
as primer on ATR.
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I am new to NMR analysis.
What I wish to do is an untargeted approach (i.e. no compound identification), using standardized spectral binning.
This should be possible and in theory pretty straight forward in the CHENOMX software.
However, the values in the output file seems to be based on both the above and below baseline 'peaks' , I upload here an example which I hope illustrates the issue.
What am I doing wrong? I will greatly appreciate any feedback to this question.
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..hmm..conceptionally you are right, but what would happen to signals so small that they remain completely below the baseline (see e.g. duplett of duplett (dd) and singulett (s) left and right of your signal of interest - if you were interested in those)...I'd regard such a approach "dangerous" - and would recommend properly processed spectra!
Alfred
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We are currently trying to perform spectral analysis on blood pressure with matlab. The device we used(Caretaker, Biopac) provides time position and amplitude of the peak according to the PDA model. The inter-peak interval was calculated by subtracting the time position of successive peak.
However, the interval between peaks were not uniform. We found that the process called interpolation should be performed before using FFT. So, instead of using FFT, we tried Lomb-Scargle periodogram(Reference: https://www.mathworks.com/help/signal/examples/spectral-analysis-of-nonuniformly-sampled-signals.html). The problem is, we don’t know how to calculate the blood pressure variability of interested bandwidth based on Lomb-Scargle periodogram. As a quick fix, we used trapz function on matlab to integrate the area under the curve of interested bandwidth.
But we are not sure about the validity of analyzing process. Is it OK to use trapz function on matlab to calculate the BPV of interested bandwidth on Lomb-Scargle periodogram?
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First what are you measuring. BP has two componets, systolic and diastolic. What have you got? where is the cuff that measures blood pressure. IMO you need to look at where you get your data before you do any supermathematics. Then you might want consult an expert in chemometrics. I would suggest: Dr. Peter Harington, Chemistry and Biochemistry Dept, OHIO University, USA. Google this name to get full contact information and the ask his advice or perhaps even invite him to work with you. You may mention my name. Good luck, David Booth
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I want to perform a WRF simulation, but I am unsure whether I should spinup as I am also doing nudging. So I have these questions basically.
1. Should I do model spinup if I am doing nudging along with it?
2. Several studies show different spinup time. What will be the optimal spinup period?
3. Whether spectral or analysis nudging is best for simulating precipitation in a very complex terrain?
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If the length of the simulations are only one month, the only spin-up that needs to be accounted for is the atmospheric one, which is typically only a few days. If I understand well, you are nesting two domains, the first one at 27km resolution (which is about the same as ERA5), and the second one at around 9km. In this situation, I would suggest to use 5 days spin-up in the beginning of each nested integration (so adding up both spin-up would lead to 10 days), and then begin the one-month simulation.
Maybe you could find the following paper of interest :
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Dear all, I would like to do the following:
Calculate the heat source due to the absorption of radiation within a layer that absorbs radiation. I would like to solve that at a spectral level. Meaning that the absorption coefficient of the material will be wavelength dependent. At the same time, I would like to fix a source light with an spectral distribution. The idea is to use FEM approach.
To start simple, I would like to release a density of rays perpendicular to the material and account for the reflection at the interface due to different refractive indexes. After that calculate the heat source to to absorption. After that, I would like to add a stack of layers with different materials (refractive indexes) and calculate the heat source in each of the layers while the light travels through the different mediums. Once I achieve this, I would like to calculate the transference of heat (by conduction, convection and radiation).
I was thinking in COMSOL, although I do not find it intuitive and I am having trouble using the "Ray Heating" interface. Any one can make recommendations for software using FEM simulations or knows how to approach the optical-thermal model in COMSOL?
Best wishes!
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Dear all,
Let me briefly go through the problem I am facing.
Currently, I have data ( of ground acceleration) obtained from the "seismic accelerograph instrument system" which was placed at the basement of the building and the plot is shown below. According to the plot, it is showing a random waveform up to a certain time and it starts decaying (damping occurs). However, it again gets another waveform (sinusoidal, as shown in the figure) after 300 sec. It looks very unusual to me. I suspect the sinusoidal part to be a building response. But I couldn't decide whether my assumption is valid or not.
So, my questions are:
  1. Is there anything (books/journals/published or unpublished thesis/lecture notes) that talks about the limitations of the time period which we are supposed to make while plotting the ground motion data?
  2. Is there any specific guidelines or any thumb-rule to determine whether the certain waveform is coming from the earthquake motion or is a building response? Normally, what I do is- I consider the random waveform as an "earthquake response" and a sinusoidal waveform as a "building response". Is it the correct way or is there another way we need to look at?
  3. My confusion arises when I saw a portion of "sinusoidal" wave before there is damping. In the figure, it is shown under the "orange" box. So, is it acceptable if I make a statement like- the presence of sinusoidal wave along with the random wave is due to the fact that the sensors recorded the both "earthquake and building response" at a time?
  4. If No, how can it be justified? If Yes, how do I correct this problem?
Thank you so much.
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There is free software which will do this, as well as adjustment and filtering, for you.
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I would like to calculate the monthly average of the representative solar spectrum for each month based on minute spectral irradiance measurements. Can I consider this hypothesis? Has anyone made this assumption?
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Dear Luciano Neves
From my point of view, it can be considered, but the end result will be inaccurate and approximate because it will depend on many variables as Professor Abdelhalim Zekry mentioned it above,
For more details please take a look at the attached files
Best wishes
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Hi everyone,
Usually finding the sample position in bright field is easy but when we change the microscop to the spectroscopy setting, my sample got lost. Does anybody has a solution for this problem?
Thanks alot for your help
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Hello Elmira:
I recommend you to use gridded glas coverslips. You can search Google for "gridded glass coverslips" to find the type and brand that suits you.
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should the reflectance data be resampled to a sensor?
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By asd device you will get .asd file and you can convert that ascii asd file to txt file with help of viewspcpro software. Then import that data into excel sheet.then you can calculate any SVI.
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I have examined two compounds band gap having same pyrochlore type structure but one contained carbonate group in the vacant place of pyrochlore structure having negative band gap (-0.22 eV) but other one have no carbonate group with band gap 0.2 eV.
Why this compound exhibited negative band gap?
Could carbonate group influence the band gap?
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When it comes to the determination of an absolute valence of the band gap, the usefulness of these Tauc plots is very limited. You can use it for a qualitative study, in your case maybe something like "X has a band gap lower than Y", but keep in mind that, depending in the quality of your data and also on what you know about your material, you may introduced an error of 200-300meV easily.
As Jürgen said, use other quantitative methods to substantiate your result. Spectroscopic ellipsometry and modelling is usually working well for me.
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The minimum number of RR intervals required for reproduce several metrics derived from HRV (e.g., HF power) can be found in the literature (Richards et al., 2010). However, what about PPG signals and the Pulse Rate Variability? Since PPG was proposed as a surrogate of ECG for the analysis of HRV, is there a minimum number of PP intervals required for reliable and accurate derivation of the PRV?
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There is no difference between the number of PP and RR intervals to perform short-term HRV analysis. Both types of information represent essentially the same process - time intervals between heart contractions. As to the number of intervals needed for the analysis, it depends on what HRV parameters you want to calculate. For frequency-domain analysis, it would be more accurate to determine the length of recording in seconds rather than the number of intervals due to the nature of spectral analysis (assumed that FFT analysis will be used). It should be enough to record PP intervals for 5 minutes to estimate HF and LF. But it would be better to record intervals for 10 or more minutes to reliably estimate VLF.
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1) I would like to ask you about a criteria from your experience to help me decide on the values constituting the background noise that I should suppress from my signals while doing data analysis of data acquired via spectrometer (Intensity counts and wavelength). If I have 4/5 spectra I want to make them start from zero.
2) Is there a formula (set of formulas) that take (s) into account the dependency of the spectrum (wavelength drift) with respect to frequency, voltage and temperature ?
Thank you very kindly and in advance for your contributions.
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Where could I find a MATLAB code for estimating the PRV-high frequency (0.04 - 0.15 Hz) power from a PPG signal? Thanks in advance!
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Hi
The methodology (code) is not different from HRV analyses having RR-interval from ECG.
fs = 4;
time = (Rtimes(1):1/fs:Rtimes(end));
IBIint = interp1(Rtimes,IBIs,time','spline')';
y = detrend(IBIint, 'linear'); % you can apply different detrending methods
window = min(300*fs, length(y));
noverlap = window/2;
nfft = max(256,2^nextpow2(window));
if rem(nfft, 2) == 0
DFT = (nfft/2)+1;
else
DFT = (nfft+1)/2;
end
% you can decide which DFT you want for example DFT = 0:0.001:2;
% for AR metod
order = 20; % you can use different order
[Pyy, f] = pburg(y,order,DFT,fs, 'onesided');
% for FFT method
[Pyy, f] = pwelch(y,window,noverlap,DFT,fs,'PSD','onesided');
VLF_ab = sum(Pyy(f >= 0.003 & f < 0.04));
LF_ab = sum(Pyy(f >= 0.04 & f < 0.15));
HF_ab = sum(Pyy(f >= 0.15 & f < 0.4));
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proper tool for converting the spectral data and ocr tool for it and if any case studies regarding it
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Dear Mohammend,
Nowadays there are many softwares to get a good spectrum.But the softwares used in the spectrometers themselves are the best. You should get academic version of the softwares to manipulate your datas. Usually the academic version is free.
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I am working in the field of metabolomics, we don't have any licensed software, I tried even the MNOVA free trial software. Kindly suggest me any other free software for NMR data analysis in metabolomic research.
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ACDLabs used to have a free academic edition. I use it for standard NMR data analysis. Though I have no idea what metabolomics you can give it a shot (attached here)
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I'm trying to use Mettler Toledo's IC Quant software to generate calibration models for the reaction components. I run my reactions at high temperature and pressure, since I cannot collect the reaction standards needed for the calibration at the reaction temperature, I prepare the reaction standards first by running the reactions to different conversions of my limiting reagent (so that I have different concentrations for the components). I then collect the spectrum of these reaction standards at room temperature and use these spectra and the measured GC-FID  concentrations for multivariate data analysis. 
Now the problem is, the absorptions are becoming less intense with increasing temperature. Hence when I try to apply the calibration model (built using reaction standards collected at 25 C) to the real-time reaction spectra collected at the reaction temperature of 140 C, I see a significant offset in the predicted concentrations from that of its actual value (the predicted concentration have negative values). I also notice that the temperature dependence is linear in the range that I tested (25 - 140 C). I'd like to to know if there is a standard procedure to apply the temperature correction to the spectra collected at a different temperature in real-time to get accurate predictions for concentrations.
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A physical law is always good but I thing that an empirical correlation that you found under your experimental conditions with your specific materials is better. When I do FTIR-ATR experiments I prefer my calibrations over external ones like PNNL and I would prefer using it also over theoretical ones (but maybe that's just me)... good luck
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Hello,
I need guidance to find harmonics of complex and real time sound captured by four Microphone array?
I have data set of drone flying operation, i have localized sound sources that have drone sound and noises.
I want to detect drone because most of frequency components are consisting of drone, by estimating harmonic frequencies i can make guess for drone sound.
Fs = 32000.
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I designed function of above algorithm but i'm unable to specify the threshold frequency Ft and N.. i just know sampling frequency of drone sound data. Arpit Jain
function f=fre_harmonic(s,fl,fr,ft,N,fs)
%fs: sampling frequency
FFT_s=abs(fft(s,N));
fl1=ceil(fl*fs/N); %Transform Frequency to Points + inf
fr1=floor(fr*fs/N); %Transform Frequency to Points - inf
[v,f(1)]=max(FFT_s(fl1:fr1));
for n=2:N
fl1=ceil((n/(n-1)*f(n-1)-ft)*fs/N);
fr1=floor((n/(n-1)*f(n-1)+ft)*fs/N);
[v,f1]=max(FFT_s(fl1:fr1));
f(n)=f1+fl1;
end
Kindly help me so that i may get able to complete above mentioned process in main question.
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can anybody please help me determine how i can obtain the zonal acceleration from reference PGA of 0.323 for class site B?
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Interesting
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I made a response spectrum analysis in Ansys Workbench and I would need to know the linearized stress components for further validation, but only the Von-Mieses stresses are available in solution toolbar.
Has someone solution for this? Maybe user defined results, PRSECT command, or export the results of RS analysis to structural one?
I am trying with these, but I could not figured it out yet...
Thanks!
Jozsi
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In my opinion when response spectrum analysis is used, the problem of evaluating Von Mises stresse or perming linearization is tricky. The stress tensor at a point resulting from RS analysis has components which (1) do not occur simultaneously and (2) have lost a physical sign. So folks...
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Hi
I want to know the exact functional groups for my FTIR Spectrum , the peaks were located at 1048,1073,1239,1256,1276,1333,1428,1554,1638,2854,2926,2961 &3421
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I have the data of total dissolved soilds of apple as references (y-variable).
I also have near-infared spectra data as predictors (x-variables).
I have the StatSoft Statistica software for the analysis.
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Different related software's can be used for building ANN predictive model using NIR spectra. My suggestion are Unscrambler and IBM modeler. Before ANN modeling, PCA should be done to reduce large spectra variables to PC1, PC2 .... . after calibrating ANN, you have predicted values by calibrated model and you have also reference values for each sample. Now use RPD index to realizing the goodness of your calibrated model.
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I have been scanning UV-Vis spectra on a Genesys 10S & have saved the *.ss data files onto a USB. However, my computer is unable to open them. The VisionLite 5 software from Thermo Scientific costs around $700, so is not really an option for me...
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Try "Spectragryph" from Spectroscopy Ninja. The software accepts 61 file formats. https://www.effemm2.de/
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Could someone help me - which software do I need to read lsjpg/lsjpi file formats? This seems to be a proprietary format produced by thermal imaging cameras.
I can't find much information about them on the internet and its proving hard work tracing the equipment/camera used to produce them as well.
Any guidance with an existing program or methodology to decipher them would be most helpful.