Anhui Institute of Geological Experiment

Hefei, China

Anhui Institute of Geological Experiment

Hefei, China
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Zhang X.,Chengdu University of Technology | Wang Y.,Chengdu University of Technology | Wu R.,Anhui Institute of Geological Experiment
Journal of Natural Disasters | Year: 2017

A series of large-scale mass of debris flow have been caused by continuous heavy rainfall after the Wenchuan earthquake in the Qingping township, Mianzhu City and three times larger scale of debris flow have broken out in Yumaipengzi Valley, especially. It caused a certain degree of loss for the plant and equipment of Xiaomuling Hydropower Station, life and property safety of power station staff also suffer a serious threat. Based on the field investigation and comprehensive analysis of basic characteristics and formation conditions of the debris flow, the risk assessment and the possibility analysis of blocking river were carried out. The results indicate that the characteristics of Yumaipengzi Valley debris flow is viscous, and integral scale of the debris flow is medium; the topography, structure and material source of the basin are favorable for the formation of debris flow, especially the possibility of occurrence of debris flow again under the action of heavy rainfall; the risk assessment result of Yumaipengzi valley indicates that the valley has middle risk of occurrence of debris flow; through the calculation and analysis, in case of rainstorm of 10-100 years return period, the occurrence of debris flow will result in blocking the river, even completely blocking the main channel.


Wang Y.-P.,National Research Center for Geoanalysis | Xu C.-X.,National Research Center for Geoanalysis | Dai A.-F.,National Research Center for Geoanalysis | Dai A.-F.,Anhui Institute of Geological Experiment | And 2 more authors.
Geological Bulletin of China | Year: 2012

The measurement uncertainty of the analytical results of B in groundwater samples by inductively coupled plasma-mass spectrometry (ICP-MS) was evaluated using continuous propagation model of uncertainty and the regression of x, y double error was used in the course of standard curve fitting. The main sources of measurement uncertainty include the sub-uncertainties of standard stock solution, the preparation of the standard series solution, repeated measurements and the fitting of standard curve. Compared with the uncertainty results obtained by the least squares linear fitting, the results obtained by the regression of double error are more accurate for relatively high concentrations.


Dai A.-F.,National Research Center for Geoanalysis | Dai A.-F.,Anhui Institute of Geological Experiment | Xu C.-X.,National Research Center for Geoanalysis | Yuan J.,National Research Center for Geoanalysis
Geological Bulletin of China | Year: 2012

The measurement uncertainty of the analytical results of phenol in groundwater samples by 4-Amino antipyrine chloroform extraction spectrophotometry was evaluated using continuous propagation model of uncertainty. The standard uncertainty of a groundwater sample was evaluated and the expanded uncertainty was calculated, which shows the measurement is credible. The results show that the uncertainty caused by the curve fitting and the sample preparation makes a relatively great contribution to the expanded uncertainty.


Wang Y.-P.,National Research Center for Geoanalysis | Pan H.,Heilongjiang Institute of Geology and Mineral Test and Application | Xu C.-X.,National Research Center for Geoanalysis | Dai A.-F.,National Research Center for Geoanalysis | And 3 more authors.
Geological Bulletin of China | Year: 2012

The measurement uncertainty of the analytical results of Ag in groundwater samples by inductively coupled plasma-mass spectrometry (ICP-MS) was evaluated using continuous propagation model of uncertainty. The regression of double error was used in the course of standard curve fitting. The extended uncertainty of measurement results was obtained from the synthesis of uncertainties from each source. When the silver content of the actual samples is relatively low, the uncertainty generated in the course of standard curve fitting is comparatively large and even becomes the dominant factor.


Xu C.-X.,National Research Center for Geoanalysis | Zhang Z.-E.,Bureau of Mineral Resources | Wang Y.-P.,National Research Center for Geoanalysis | Dai A.-F.,National Research Center for Geoanalysis | And 3 more authors.
Geological Bulletin of China | Year: 2012

The measurement uncertainty of the analytical results of sulfides in groundwater samples by para-amino aniline photometric method was evaluated using continuous propagation model of uncertainty. At the key step of standard curve fitting, the authors adopted the double-error curve fitting in comparison with the least square method. The results show that, for the higher concentration samples, the results of double-error curve fitting are more accurate, and when double-error curve fitting is adopted to quantify the actual samples, the appropriate concentration range of standard curve should be selected, in which the concentration of the samples falls into the range of higher concentration, so that the results are more accurate and reasonable.


Yuan J.,National Research Center for Geoanalysis | Wang Y.-P.,National Research Center for Geoanalysis | Xu C.-X.,National Research Center for Geoanalysis | Wang S.-M.,National Research Center for Geoanalysis | And 2 more authors.
Geological Bulletin of China | Year: 2012

The measurement uncertainty of the analytical results of T1 in groundwater samples by inductively coupled plasma-mass spectrometry (ICP-MS) was evaluated using continuous propagation model of uncertainty. The regression of double error was used in the course of standard curve fitting. The extended uncertainty of measurement results was obtained from the synthesis of uncertainties from each source, but the uncertainty from pretreatment procedure was not considered. When the thallium content of the actual samples is relatively low, the uncertainty generated in the course of standard curve fitting is comparatively large and even becomes the dominant factor. When the content of thallium is high, the uncertainty from standard curve fitting is relatively insignificant.


Sha L.,Anhui Institute of Geological Experiment | Sha L.,Guilin University of Technology | Ren C.,Guilin University of Technology | Peng J.,Guilin University of Technology | Wen H.,Guilin University of Technology
Journal of Geomatics | Year: 2011

The estimation method and the function choosing in de-noising of wavelet threshold are introduced, and comparative analysis of threshold function choosing is presented. Based on observed data from Ertan Dam in Sichuan Province, comparison between original and estimated signal after de-noising on evaluate index of SNR and MSE is proposed. According to theoretical analysis and engineering projects, the almost-hard thresholding can be more effective to take the local deformation characteristic information than Garrote thresholding.

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