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Questions related to DRIFT
Somewhere in the world there must be a bunch of scientists working to establish a more accurate value for the mass of the electron.
NIST publishes an updated value every 5 years, so I assume someone is doing the measuring.
This field is of great interest to me, as my hypothesis predicts a slowly drifting electron mass.
If anyone happens to know someone directly or indirectly, I would love to have a contact.
For example, I have a single mode fibre based Mach-Zehnder interferometer, when I put it into a temperature stablised enviroment, there would be a linear phase drift? What is the phase drift at different temperatures? Is there any paper talking about this?
Does anyone have insight as to whether it's possible for K-internal to go bad?
We are performing whole-cell patch-clamp recordings. For the past few months we have been having issues with cells dying shortly after forming a gigaohm seal and breaking in. I can only hold a cell for 10 minutes or so. We have checked pipette drift, the pipette isn't drifting. Our slice quality is fantastic. The only other factor we can think of is internal solution. All of our internal is made, dated, placed in hundreds of small containers, and only one or two containers are thawed on the day it's time to patch.
At this point I've patched onto hundreds of neurons with this problem, statistically at least one should have survived past 10 minutes but none have.
Is it possible for K-internal to go bad?
Apps such as https://chat.openai.com can now collate diverse information in response to a question and compose well phrased readable essays. The are likely to become more capable over time and through better ‘algorithms’ and larger training datasets.
Possible impact areas (more please) :
- ethics
- the process or craft of research
- academic institution processes
- how academic research is owned and monetised
- the drift of academia‘s attention moving to what the apps best facilitate
Hello,
I have been following the Drift method for my chars (0,1M NaCl solution and pH adjusted with 0,01-0,1M NaOH/HCl) by adding 50mg char in 50mL of a 0,1M NaCl solution pH adjusted.
One of my main problem is that the pH final is always above (except for 11,03 where the pH final was 11) the initial pH. I have been doing th range of 2,5 - 11,3 and I can't find a really big tipping point. What am I doing wrong? Is it my NaCl solution that is too concentrated?
Thanks !
Dear all,
I have been trying to use ArtRepair and I have some questions regarding the preprocessing I am doing, and I would be very grateful if you could answer some of them. The preprocessing I am doing is as follows:
1. “art_slice”: Normally the threshold has to be modified until it is inferior to 5%.
- IS IT OKAY IF THE THRESHOLDS ARE DIFFERENT FOR DIFFERENT PARTICIPANTS?
- WHAT TO DO IF THE MASK CREATED IS NOT ACCURATE (THERE SEEMS TO BE DATA OUTSIDE THE HEAD)?
2. Slice timing
3. Realign & reslice
(4). art_despike IF “visual inspection of the ArtGlobal figure uncovers greater than +/-1 % drift in the mean global signal across the entire time series”.
- IS THERE A WAY TO CALCULATE THE PERCENTAGE OF THE SIGNAL DRIFT IN ORDER TO CHECK IF IT’S GREATER THAN +/-1 %? (For example by calculating the % of decrease between the maximum and the minimum value OR the first and the last image?
5. Coregistration
6. Segmentation
7. Normalization
8. Smoothing
(9). art_global: apply if art_despike was not applied.
When using art_global, users are asked “always repairs 1st scan of each?”. IF I ALREADY DELETED THE TWO FIRST DUMMY SCANS, SHOULD I REPLY “YES” OR “NO”?
- IF THERE IS TOO MUCH MOTION, IS IT OKAY TO SKIP “art_motionregress” AND USE THE “.rp” FILE FROM THE REALIGMENT STEP AS MOTION REGRESSORS?
- WHEN USING MOTION REGRESSORS, IS IT BETTER TO LEAVE THE SCAN-TO-SCAN MOVEMENT THRESHOLD AT 0.5 mm/TR?
- IS IT A PROBLEM IF ART_DESPIKE IS PERFORMED FOR SOME PARTICIPANTS AND ART_GLOBAL FOR OTHERS?
Finally, I would like to know if you believe the preprocessing I described is correct or not.
I would be extremely grateful if any of you could answer to these questions, it would be very helpful!
Best,
Ariadna
Also, when do we use unit root (ADF) with trend and unit root with drift?
I need maximum force in every drift in one Composite Shear Wall(CSPSW). I utilized dynamic Explicit and apply cyclic loading . I obtained hysteresis curve of my analysis. But how can I procure backbone curve out of analysis outputs?
Keogram is a analysis technique used in all sky images to demonstrate the E-W and N-S information from the images.
E-W keogram gives the longitudinal offset information of the plasma bubble drift and N-S keogram gives its latitudinal variation in intensity as well as it provides the meridional drifting if any.
We plot this keograms in MATLAB where you get the options as RGB, Grayscale etc. Which option is scientifically correct as far as the all sky imager analysis is concerned?
I use grayscale, but sometimes using RGB option gives complicated plot, in which it is very difficult to track the bubble movement.
Thanks.
When you speak of damage, is it the apparent cacking, residual, permanent distortions, the roof level drift, or the invisible concrete pulverisation, lap splice failure or rebar slippage or something else?
How can we reduce the breakdown voltage drift of Insulated Gate Bipolar Transistor (IGBT) after 1000 hours of HTRB reliability test? For instance, the BVces dropped from 1590V to 1450V after HTRB.
what causes Breakdown voltage (BVces) to drift after HTRB reliability test? I do understand HTRB is an accelerated test which eventually leads to carrier's mobility degradation in the field depletion structure. But what is the main reasion causing BVces to reduce from 650V to 550V after 1000 hours?
is there any recommendation to reduce the decrease the BVces after HTRB test?
Hi, recently I am trying to correct the baseline drift for the targeted FFA LC-MS method. Our system still use a HPLC so I have to downgrade one of the UPLC method. All the mass are fine, but I see a gradual baseline drift for mass C16:0 (Neg, m/z=255.23) and a suddent uprise of the basline for mass C18:1 (Neg, m/z=281.25).
Currently, the method is setted as following:
Column: Gemini® 5 µm C18 110 Å, LC Column 250 x 2 mm, Ea
Solvent A: 3:2 (v/v) acetonitrile/water containing 10mM ammonium acetate
Solvent B: 1:1 (v/v) acetonitrile/isopropanol (this in origianl method have 10mM ammounium acetate as well)
Gradient is : 1ml/min SolventB 0min, 10%; 1.7min, 10%; 11.9min, 35%; 14.9min, 100%; 17.9min, 10%; 20.0min, 10%. Pressure is highest at 275.4 bar (3994 psi)
I am reading a bit for this fixing, and also for the system limitation. And here is some of the change that I think of that might help me with this.
1. The pump we use is Agilent 1260 G1312B, the pressure range is 0 – 600 bar, 0 – 8700 psi, but my collegue and I keep having problem if we run above 3000psi, so one of the change I am thinking is to reduce the flow rate to 0.6 or 0.8 ml/min
2. I know the ammounium acetate does not dissolve in ACN or Isopropanol, so 100%B in the gradeint is probably bad for the column so I am decreaseing the %B to 95%.
3. The ammonium acetate alone can only be a salt solution and it's not properly buffered. I will try add (0.05% or 0.5%) ammonium hyrdoxide or acetic acid to properly buffer the solution.
These are some of the change that I want to make that from my understanding will be a better practice for the LC run, but I haven't seen clear clue that one of these change will definitely help fix the issue that I am having right now which is baseline drift for paticular mass.
Thus, I am wondering if I miss any points or anyone have similar situation before and how did they fixed it. I also add a figure to show the two
Dear all,
I' m facing some problems with my western blot. The bands of markers seems normal in the gel after electrophoresis, but they drift after transferred to the membrane (showing in the picture)? Does anyone know what could be the reason? I've met this a few times.
Thank you so much!
What is the origin of the shift (up) in the baseline of the UV-VIS spectrum as noticed from 300 nm to 800 nm in the screenshot attached? I'm measuring phenobarbital in 0.2 NaOH against 0.2 NaOH blank. I have tried turning off fluorescent lights, CRT monitors, and capping the cuvette while measuring the sample on my HP 8453 chemstation.
Hi,
I'm doing an EEG analysis from a collaborating University so I did not collect the data myself. The few of the recordings show a giant drift/wave across many of the channels which is something I have not come across before (attached is a picture). Does anyone know why this artefact occurred? And is there a way to save the recording or should I discard them?
Data has already been downsampled / filtered
Antigenic drift with typical 'ladder-like' phylogeny has been observed with multiple lineages in Influenza(Flu) which makes it more predictable and aids in vaccine development on a yearly basis . With Omicron variant also showing similar ladder like phylogeny with XE variant a hybrid of Omicron BA.1 and BA.2. Is it a good sign for the future implications and predictability?
I used two samples, one of pure SiO2 and one of pure Al2O3. For each sample I obtained the corresponding ATR (attenuated total reflection) and DRIFT (diffuse reflection) spectra. The spectra look very different from each other, they seem to be from totally different samples. What can this be due to? For both measurements I used an FTIR spectrum of KBr as Background under the same conditions of each measurement.
Spectrometer: Nicolet™ iS50 FTIR
Spectral range: 4000 – 400 cm-1
Resolution: 4 cm-1
Background and sample scan: 32
Zero filling factor: 2
Apodization function: N-B Stark
Phase correction mode: Mertz
Detector: DTGS ATR
Beam splitter: KBr
Background and sample signal gain: Auto
Mirror velocity: 0,4747 cm/s (ATR), 0,0317 cm/s (DRIFT)
Aperture setting: 100 (ATR), 200 (DRIFT)
Accesory ATR: Smart iTR™ Attenuated Total Reflectance (ATR) Sampling Accessory
Accesory DRIFT: The PrayingMantis™ diffuse reflection accessory (Harrick Scientific Products)
My group is considering getting a new oxygen sensor for peatland soils and soils under thawing permafrost conditions. Our current sensor (Pyroscience) works well in water and in air, but has issues in a soil matrix (the value needs a long time to stabilise and starts drifting off soon after). Plan is to use it for measurements during the field work, no long time observation (for now) necessary. I appreciate any experience shared and/or recommendations.
How one can learn independently Simulations like drift and diffusion modelling and many other relevant simulations .
I have been performing experiments in which I weigh polystyrene or polyurethane in an analytical balance, but anytime I place my sample, the weight keeps going down and does not stop. I read that probably is a problem with the static of the sample. Has anyone encountered this problem and knows how to deal with it?
Thank you
Now a days because of non availability of labour the usage of pre & post emergence herbicides is more among the farmers. But sometimes due to the herbicidal drift most of the farmers are facing the problem of tip drying, crinkling and sometimes completely drying of the plants. Can anyone please suggest the best management methods to recover the plants from herbicidal drift.
Hello,
I have a one cycle of hysteretic curve which has so much less width that it doesn't look like a cycle as it just looks like a line. I want to find area of that loop. I have tried to find the area in origin-lab using various techniques and it comes to be 4 approximately. I just want to confirm that whether this area calculation in correct or not. Please, anybody that have used origin-lab and can find the area between the loop easily, confirm it. Excel sheet is also attached with drift on X-axis and Base shear on Y-axis. P.S base shear is in units of pounds (lbs) and drift has no units then what would be the unit of this calculated area?
Thank you
Genetic analysis of the COVID-19 virus shows that it is very similar to a coronavirus in bats but the receptor binding looks like the receptor for SARS. This could happen naturally with slow changes of one in ten thousand sequences each year. This appeared all at once. This gives support to the belief that the Wuhan lab took the bat virus and attached the SARS receptor. So, does the COVID-19 show antigenic shift and drift?
Hi dear friends,
Would you please guide me through calculating the wind-drift according to CSA load combinations?
That is to say, What are the load combinations shall be used to obtain wind drift?
thanks for your time in advance,
mohamad
Hello everyone!
I'm trying to replicate analysis 1.3 from the paper: "Phylogenetic analysis of a new morphological dataset elucidates the evolutionary history of Crocodylia and resolves the long-standing gharial problem" of J.P.Rio and P.D.Mannion. With their supplementary files "Raw data: TNT file with continuous and discrete morphological characters (used in Analysis 1 and 3)." and the following protocol :
piwe=
open the matrix
piwe=12 ; (weight of 12)
xpiwe= ; (active EIW)
piwe; (see if all is ok weight of 12 and EIW ON)
Then NewTechnologySearch with :
- on letf side : Sect Search + Ratchet + Drift + Tree fusing (on default setting)
- on right side : Driven search with init addseqs of 5 + Stabilize consensus 5 times with 75 factor
Random seed of 1 and Auto-constrain and replace existing trees ON
Then TBR with Tree on ram.
But I get a tree with the best score of 8900 something whereas in the paper the best score is 8181.9.
Does someone have an idea where I mistaken?
I have a Steel structure that It has three axes in the x-direction and y-direction. I enter displacement load the head of each column, and I push with 8% drift. When I turn on Nlgeom in step, my chart( force-displacement) does not have nonlinear steel behavior, and in the plastic region, Many forces develop in my chart. It causes my columns to be plastic, but I do not turn on Nlgeom, the nonlinear steel behavior is good, but I do not see local buckling in my beams.
What is the cause?
Could someone give me an indication of drift limits provided if any for in-plane flexural or shear failure of URM piers in NZSEE/Seismic Assessment of Unreinforced Masonry Buildings Section C8 ?
Hi,
I acquired multiple confocal stack images of olfactory epithelium from rostral to caudal position from 1 slide. I want to create 3d reconstruction by adding all the z stacks to look at expression pattern of few neuronal markers. I am able to add multiple stacks by selecting "add slice" option. However, there is a distance of 50 micron between every 2 slices. 2 questions:
1) Can I add blank space of 50 micron between every 2 slices?
2) How to align for x-y drift between different z stacks?
Thank you
Raghu
Citing Surendra Adhikari at NASA, I would like to ask how it is possible to claim that the North Pole drift is caused by climate change:
"Climate change does not only cause the rise of the oceans, it also disturbs the magnetic field of the Earth.
"There has been a dramatic change in the direction of pole drift, undoubtedly caused by climate change, which is linked to the disappearance of the ice sheets,
especially in Greenland," said Surendra Adhikari, researcher at the NASA. The North Pole has lost 278 gigatonnes of ice since the beginning of the third millennium.
As a result, the magnetic north pole moves eastward, and faster than before. The melting of ice would account for 66% in the acceleration of the phenomenon."
The magnetic pole drift is caused by the magnetic field strength of the North American flux lobe and the Siberian flux lobe (Ref: 1, 2, Figure 1). This is also based on a comparison with the magnetic South Pole in Antarctica, which is immobile and entirely surrounded by ocean, while the magnetic North Pole is driven by continental mineral density of the two major continents forming large magnetic fields. These mineral densities of the Siberian and Canadian regions are fluctuating with the activity of the internal core and the rotation of the iron core of the earth, seismic activity and change in mineral composition of the mantel over several years. The geomagnetic properties of these region can change drastically by the alterations of the electromagnetic field of the planet Earth, which is also affected by the electromagnetic field of the Sun. How can NASA claim that the North pole ice, which is virtually the same as water around Antarctica in magnitude of electromagnetic strength, alter the position of the magnetic North Pole?
References.
1. Gubbins, David, and Peter Kelly. "Persistent patterns in the geomagnetic field over the past 2.5 Myr." Nature 365.6449 (1993): 829.
2. St-Onge, Guillaume, and Joseph S. Stoner. "Paleomagnetism near the north magnetic pole: a unique vantage point for understanding the dynamics of the geomagnetic field and its secular variations." Oceanography 24.3 (2011): 42-50.
I have seen an example of tracking position in one dimension using an alpha beta filter, and I have a similar problem in a different field. In the example the position is first updated via dead reckoning: New position = old position+ velocity times delta t. Then the new measurement is used to update both the position estimate and the velocity estimate using the alpha and beta weights. I would like to see this problem formulated using a Kalman filter. I think I can come up with the variance estimates required and prefer this to somewhat arbitrarily selecting alpha and beta weights. The change in velocity is a drift, i.e. not driven by any known input.
I have an ICP-MS measuring metals in drinking water. Dissolved Ca precipitates on the cones and causes a decrease in instrument response quickly over time. For example, only 10 samples of high-Ca water will cause a 15% decrease in instrument response. I can follow the decrease in response by running check standards every 10 samples. Is there a way to re-calibrate the slope (or 'reslope') every 10 samples by re-measuring only one standard solution, instead of re-calibrating (10 cal standards) every 10 samples? Or is there another way to correct for drift?
I use a mechanical translation stage with a retroreflecting mirror as a delay line (fs laser - gate(pump)). Despite the retroreflecting mirror ensures getting parallel beams (in & out beams), I noticed a laser beam drift when I scan the translation stage over relatively long distance, i.e. approximately 100 mm back or forth from the mid-point.
I know this can cause troubles for my experiments, particularly I use collinear geometry for pump(gate)-probe experiment, hence both beams must coincide without deviation upon scanning the delay line.
Can any one please tell me, how can I correct that ?
We are seeing our QC check standard for nitrogen decreasing significantly after batches of 20 runs. The first check is 98 ppm, the next 82 ppm, the next is 70 ppm, the next is 51 ppm and the last one was 34 ppm.
Wondering why the check is slowly being decreased. Is there a way to adjust something in the instrument? thanks.
I would like to learn how to choose the L and C values in a DSRD based pulse generator circuit. What modeling software can help me do that and determine the waveforms as functions of the L and Cs? In other words, in Figure 3 of the article "4H-SiC Drift Step Recovery Diode with Super Junction for Hard Recovery" by Xiaoxue Yan , Lin Liang *, Xinyuan Huang, Heqing Zhong and Zewei Yang in Materials 2021, 14, 684 they show the L and C values. SInce I am a novice in pulse generation, can anybody please point to any article that discusses how the circuit would be impacted with different values of C and L? Thank you so much.
Hi guys,
We have been doing single molecule TIRF experiments with virus protein Gag to look into its assembly process. When analyzing the data, some traces look nice, but some have this baseline drifting problem. We tried some optimizations but the problem is still there. We have problems in:
1) as shown in Fig 1 attached, we think there is a clear baseline drifting (signal gradually decreasing around 0 intensity), and
2) in some of the slides, the overall signal is very intense for the first couple of seconds (Fig 2 attached), and then the image gradually become more "normal" (Fig 3 attached). This has been making our data processing process very difficult, and we are not sure if this is also related to the baseline drifting problem.
The buffer we are using contains 100 uM propyl gallate, 2 mM DTT and 4.5 mM trolox. We are kind of new in single molecule TIRF, and would really value expert opinions in how to improve/optimize the system.
Thanks in advance for any input! We really appreciate your help!
The zero drift can be seen in the attached files.
Why Moment Resisting Frame Drift is more than Shear Wall Frame Drift, if they are in the same Seismic zone and the same quantity of material?
- Analyzing two Models ( Moment Resisting Frame and Shear Wall Frame) by Etabs.
- The same property and the same quantity of materials.
- Analyzing both Models in the same Seismic Zones.
- Both Models are the same geometry, the same height and Floors.
My question is:
Why Base Shear and Drift in Model of Moment resisting frame provided more than in Shear Wall Frame?
I am looking for brain vessel image correction. I do video recording in slices of capillaries and I have some xyz drifts. Is anyone know movement correction solution preferably in imageJ
I am new in plugins use. I found Manual_Drift_Correction-1.0.0.jar.zip plugin and install it but when I trying to start it I got error: plugin or class not found and (java.lang not found.
Please help.
Thank you in forward
Ivan
What is thermal drift and what are its causes ? I did nanoindentation of a polymer nanocomposite. To know the thermal drift, at the end of unloading, low load of 0.01 mN was held constant for 70 seconds. There was not any pattern, the depth increased and decreased and at the end the depth was same as it was in the beginning. How to correct for thermal drift in such a case ? If there was only increase or decrease, i could have fit a line or curve to it and correct the displacement readings accordingly. But since there is no any pattern to it what shall I do ?
When I'm doing my indentation experiments I choose the central point on the virus to be indented but when the process ends, the force-distance curve does not represent the central point that I chose. I try to manage the image size or sonde velocity but it doesn't work very well.
Does anybody have experience how to measure the point of zero charge of buffering materials (e.g., Mn oxides, zeolites, etc. in our case)? The common pH drift method is giving us very weird results, as the materials are strongly buffering the pH to their natural pH. E.g., birnessite, whose pHzpc should be according to the literature between 2 and 4, results in pHzcp of almost 10 when measured by the pH drift method, the similar case with zeolites....Also potentiometric titrations are giving us these highly alkaline values close to the natural pH of the materials....
Don´t you have a recommendation for any other method suitable for this type of materials?
Thank you very much.
I've been using the SFI MVLEM element in OpenSees. I conducted cyclic analyses on 3 different experimental walls to verify the response from SFI MVLEM before conducting analysis on a 10 story RC wall building. I successfully verified the experimental response (global as well as local response) of those walls using SFI MVLEM. While conducting the analysis on a 10 story RC Wall building, I noticed that convergence fails at a very small drift of 0.5%, even with different displacement step sizes to conduct the analysis.
Any guidance on troubleshooting the early convergence failure of the analysis using SFI MVLEM would be a great help.
How to measure an optics thermal drift error in a laser measurement system(Renishaw XL80)?
Please tell me about optics thermal drift and what is the source for optics thermal drift. And How to find the value of optics thermal drift. And how to reduce it?
Numerical models have been used to explore potential long range predictivity
of coupled models using observed data. The early experiments have been frustrated
by rapid ocean model drift away from the observed state. Do your higher resolution models have the same behavior
I tried to perform a spectral matching in frequency domain . I have attached the result herewith. There seems to be a lot of drift in displacement and velocity plot for the matched ground motion. A total of 10 iteration was performed to obtain the match. Can somebody explain the reason and verify my work here ? Also, what is the permissible limit for the drift allowed ?
The ground motion used here is imperial Valley.
I need to plot normal stress v/s lateral drift. So in ANSYS, is there any option to obtain stresses for selected objects only? If so, please elaborate.
I want to calculate the the time evolution of drift velocity of a particular ion under different range of external electric field in LAMMPS. What would be the command for the same?
Please suggest for computer based system for processing of raw gyroscope data which method is more suitable for bias drift and noise removal from gyroscope? I need angular velocity in my application.
I'm trying to setup a simulation that tracks particles from a spray nozzle mounted under a propeller blade. I need suggestion on how to setup this simulation in fluent.
I'm regressing households' spending (PCE) on disposable income (PDI) between 1980 and 2018 for the U.S economy. I noticed that the coefficient of PDI is higher than 1. I first think that coeff. of PDI may be extreme due to possible autocorrelation or non-stationarity.
While conducting the ADF test, I tried the random walk, drift, and a trend.
However, according to the results of the test, PCE and PDI series are stationary with a drift.
I also applied the Gregory-Hansen cointegration test and find out that series are cointegrated in the long run at the breakpoint.
How can I solve this problem?
I observed a decrease in intensity in 4000 QTRAP (AB Sciex) mass spectrometer. It looked like a case of contamination. The standard cleaning procedure did not help. Calibration standard solutions gave peaks of very low intensities. The drift test didn't prove any contamination. Changing the detector voltage also did not help. The service checked electronics and said that it is not the reason of the problem. They suggest cleaning the quadrupoles now. Do you have any possible solutions to my problem or any suggestions?
can anyone tell me in IDA analysis, increases the scale factor of ground motion from 0.1g and upto 5g. Why the drift ratio vs spectral acceleration curve show linear , even maximum hinges show collapse point.
As it is known there is a magnetic field in large scale universe, so the particle undergoes a magnetic field will be different in case of expanding universe or static one as it will be in the trivial case; For example the drift of charged particle where it tends to spiral around a field line in this case what is the effect of the large scale on particle drift in a magnetic field
When i plot the modal pushover analysis of nonlinear fixed structure, it plotted well, but when i did same for base isolated structure, it says crossed the limit state in first few steps, what might be the reason? Can anyone explain it to me, please?
I have a question regarding the convergence problems of cyclic (quasi-static) loading for reinforced concrete slab-column connection. Is there any of you have this kind of convergence problem? I have run exactly the same model for the monotonic lateral loading and it was totally fine and gave an adequate result. However, when I change the load into cyclic then it start to diverge even for a very low drift level. I have checked all of the boundary condition and it seems totally fine.
I have a question regarding the convergence problems of cyclic (quasi-static) loading for reinforced concrete slab-column connection. Is there any of you have this kind of convergence problem? I have run exactly the same model for the monotonic lateral loading and it was totally fine and gave an adequate result. However, when I change the load into cyclic then it start to diverge even for a very low drift level. I have checked all of the boundary condition and it seems totally fine.
My question is, can you descibe what factor that may influence this convergence problem? for example, because I am using plastic compression model combined with tensile fracturing, I guess there is an issue after the concrete cracks and it start to soften in an exponential way. Do you think this kind of negative stiffness during the softening may contribute to the problem? Any suggestion and discussion will be so much appreciated.
Best regards,
Andri Setiawan
What is the reason for baseline drift of in-situ high temperature XRD pattern at relatively high temperature? Cu K(alpha) radiation was used for the in-situ high temperature XRD measurement of high purity pyrite. The baseline is straight at the temperature below 600°C, while it shifts from down to top as angle increases.
I am running an analysis that has six compounds that are evaluated for precision, linearity and drift. I have the unusual problem that drift for 5 of the compounds after analysis is ~ 20% higher, but drift for one compound, TOTM, is doubled, with a drift of 100% or more. I am using Acenaphthene-d10 as the internal standard, and response of this compound is really steady, but especially after samples are injected, the response of TOTM increases significantly. I've been working on this project for about a month, and if I look back at older data, the response of TOTM has been slowly increasing through each analysis, while the response of the internal standard has remained relatively constant. (TOTM initial response was ~ 100,000 - but now it is close to 2 million).
Some of our thoughts for the source of this problem are:
That there are active sites (or something) in the column that is causing TOTM to hang up- running the sample injections pushes that out so that more TOTM elutes in later injections.
That there is a matrix effect from the sample that increases the response from TOTM.
That the inlet is discriminating against TOTM, but then less later on? (I'm running the same method the whole time.)
Other typical players in GCMS methods are the source, the inlet, and the column, but it's still hard to see how any of those would lead to increased response from mostly just one compound.
Any thoughts? Thanks!
Dear All,
We are looking for drift velocity vs electric field of electrons and holes for finding the drift velocity saturation in the amorphous and micro-crystalline silicon.
Please guide me for the same.
Thanks,
I am looking for physics-based measurements that can be performed in the edge plasma (upstream, not at the divertor) that yield the separatrix position or some boundary for it. Some of the methods I am working on:
- measure the profile of plasma potential, find the peak
- measure density or ion saturated current fluctuation, find zero skewness (inner boundary)
- measure the profile of electron temperature, electron density, heat flux etc., fit it with a "broken" double exponential and find the breaking point (outer boundary)
- measure the profile of poloidal velocity (cross-correlation of poloidally spaced probes, Er x B drift etc.) and find the zero
Some of the methods I have found (some thanks to the answers below):
- in H-mode, fit the pedestal Te or ne profile with the tanh function and find its center (can optionally be corrected for some fraction of the SOL width) [G. Porter, Physics of Plasmas 5, 1410 (1998)]
- (specific to field reversed configurations with a weak external plasma source) modulate the plasma source at a known frequency and measure the floating potential profile with a Langmuir probe; the region where the frequency amplitude goes down suddenly is the magnetic separatrix [answer by S. Cohen below]
- assuming pressure balance along the field line, map divertor pressure measurements to upstream (at the divertor, the strike point position is known, e.g. Eich function fit, maximum heat flux etc.) and match it to upstream pressure profile (this can also be done with the floating potential, electron temperature, heat flux...) [C. K. Tsui, Physics of Plasmas 24, 062508 (2017)]
- develop some really specialised probes [K. Uehara et al, 2006 Jpn. J. Appl. Phys. 45 L630]
- use the power balance criterion (AKA Stangeby's two-point model) to calculate the separatrix temperature, then find it on any measured Te profile [H J Sun et al 2017 Plasma Phys. Control. Fusion 59 105010]
I am open to any suggestions, links to previous research, or your personal experience (whether you've encountered the problem of not knowing exactly where the separatrix is, whether you think it's worth addressing etc.).
I am wondering is there any permanent torsion limit for buildings specified in the codes? for example how much a concrete building is allowed to twist permanently (due to foundation twist or structural plasticity) after very strong earthquakes or other extreme loads in different directions causing structural torsion? For permanent lateral drift, the limit is 1% for MCE shaking but cannot find anything for acceptable level of permanent twisting angle due to torsion.
Hello, after the analysis of volcanic deposits from South-East Asia by DRIFT Spectroscopy, some peaks occur around 1300-1250 cm-1 (please see the attached image). Do you know to which mineralogical compounds they could be associated? How can we interpreted it from a mineralogical point of view? Also this shifting between the spectra (around 1300-1250 cm-1) seems like a slight variations in the crystalline structures. Do you agree?
Thank you in advance for you answers and contributions.
Among DRIFT and IRRAS spectroscopy,which one is more sensitive to detect in 1 % loading metal supported catalysis?
Because in my case, for 10 storied RC frame, drift values are coming maximum at the same node for every increase of intensity.
I would like to get suggestions for the optimal fiduciary marker for drift correction in PALM (Photoactivated localization microscopy) imaging with mEos2/mEos3.2 fluorescent protein? I was considering TetraSpeck beads, but the I am concerned about the high brightness of the TetraSpeck as this will saturate the detector when I use high laser power and camera gain for amplifying the signal of a single mEos2. Any other recommendations? Thanks
Sample is fungal and coated with Au/Pd and mounted with hot glue to the sample holder.
Image drift is worse at 5kV than 10kV
The image drift is visible on the high refresh rates used to navigate and only at higher magnifications (4500x +), but does not result in artifacts at photo quality refresh rates. If the sample was actually moving it should be represented as streaking in the low refresh rates, right?
I am viewing fixed phytoplankton cells (on cover plate) under SEM. I gold coated the sample with 30mAmp for 240 seconds and mounted the cover plate. First time when I observed the plate, the cells did not "move" at all. However, when I came back a few hours later to observe the same plate again, I could start seeing the cells on the image screen shifting at 5 um, and the shifting problem got worse when I came back to observe it the next day... The image usually moved in one direction. This prevents me from getting a high resolution picture since I cannot focus the image well. What factors can cause image shift? How can I address the issue?
The peak seismic drifts of steel MRFs are calculated by amplifying the elastic deformations due to the design lateral forces with a deflection amplification factor (DAF). The European and the Canadian codes define the DAF to be equal to the response modification factor R while the ASCE 7-10 defines the DAF to be equal to 0.6875R. Any thoughts about why there is this variance between the seismic codes.
Did Miller detect ether-drift or something else? What could the something else be? Miller suggested that the Michaelson-Morley experiment did detect the same effect as Miller but at a much smaller than expected level.
(1) Dayton C. Miller, (1933) "The ether-drift experiment and the determination of the absolute motion of the Earth", Rev. Mod. Phys., vol. 5, July, p. 203. http://www.orgonelab.org/EtherDrift/MillerRMP1933.pdf
(2) James DeMeo, "Dayton Miller'sether-drift experiments: a fresh look", www.orgonelab.org/miller.htm
I know that IBC permits to calculate story-drift based on modal fundamental time period exceeding the upper limit T. I mean that if the calculated T by ETABS exceeds the allowed upper limit for time period (Ct × H0.75×Cu), then IBC permits calculating the story-drift using the larger T obtained from ETABS.
Moreover, IBC permits to calculate story-drift without considering the minimum base shear (CS = 0.044SDSI ).
Please check the attachments to confirm these two permissions according to items 12.8.6.1 and 12.8.6.2 in ASCE 7.
I want to
1-confirm the correctness of my knowledge.
2-understand the philosophy behind this rule.. using Tetabs and ignoring the minimum limit of base shear when calculating the drift and do not allow these permissions when calculating the base shear (force)??
3-investigate if these permissions are really applied in the engineering design offices? or they are only code permissions with no use in real engineering design .