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Correlation between well logging response and TOC In Fig. 5, the abscissa represents determination coefficient; the ordinate in RD represents the response value of deep resistivity curve; TH represents the response curve of thorium content value; KTH represents uranium gamma curve response value; CNL represents neutron log response value; PE represents the value of photoelectric absorption index log response curve; GR represents gamma-ray logging curve value; AC represents wave slowness response curve; U represents the response curve of uranium content value; DEN represents the density curve of response value. It can be seen from that TOC and the density value have the biggest correlation. This is because density of kerogen (a component of TOC) is much smaller than that of other lithology. Where content of TOC is higher, density of the rock must be smaller. Of course, other curves are more or less correlated with TOC. Although there are good single correlation between some well logging curves and TOC, the goal of accurately predicting TOC still cannot be achieved. Through correlation analysis, uranium content curve (U), density curve (DEN), natural gamma curve (GR), acoustic curve (AC), neutron curve (CNL), and photoelectric absorption eoss-section index (PE) were selected as input curves; the content of TOC was taken as output. They were all normalized. Samples were randomly grouped (the samples were divided into 4 groups, each containing 33 samples.). The network parameters were all determined by the K-CV method in order to obtain an ideal fitting-model (Jiang et al 2015). In order to facilitate the comparison with other nonlinear approximation models, we attempted to write Adaboost-BP neural network model, SVM model, Kernel Extreme Machine (KELM) model and in the MATLAB software, and obtained model parameters using the samples 

Correlation between well logging response and TOC In Fig. 5, the abscissa represents determination coefficient; the ordinate in RD represents the response value of deep resistivity curve; TH represents the response curve of thorium content value; KTH represents uranium gamma curve response value; CNL represents neutron log response value; PE represents the value of photoelectric absorption index log response curve; GR represents gamma-ray logging curve value; AC represents wave slowness response curve; U represents the response curve of uranium content value; DEN represents the density curve of response value. It can be seen from that TOC and the density value have the biggest correlation. This is because density of kerogen (a component of TOC) is much smaller than that of other lithology. Where content of TOC is higher, density of the rock must be smaller. Of course, other curves are more or less correlated with TOC. Although there are good single correlation between some well logging curves and TOC, the goal of accurately predicting TOC still cannot be achieved. Through correlation analysis, uranium content curve (U), density curve (DEN), natural gamma curve (GR), acoustic curve (AC), neutron curve (CNL), and photoelectric absorption eoss-section index (PE) were selected as input curves; the content of TOC was taken as output. They were all normalized. Samples were randomly grouped (the samples were divided into 4 groups, each containing 33 samples.). The network parameters were all determined by the K-CV method in order to obtain an ideal fitting-model (Jiang et al 2015). In order to facilitate the comparison with other nonlinear approximation models, we attempted to write Adaboost-BP neural network model, SVM model, Kernel Extreme Machine (KELM) model and in the MATLAB software, and obtained model parameters using the samples 

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There is increasing interest in shale gas reservoirs due to their abundant reserves. As a key evaluation criterion, the total organic carbon content (TOC) of the reservoirs can reflect its hydrocarbon generation potential. The existing TOC calculation model is not very accurate and there is still the possibility for improvement. In this paper, an i...

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Context 1
... order to compare the models conveniently, the measurement of the TOC was carried out on 132 rock samples from the Longmaxi shale gas reservoir of the Jiaoshiba area in the Sichuan Basin (the first large shale gas field in China). With the sample points of the abnormal response value removed, the simple linear correlation of the log response and the TOC was analyzed using a crossplot single linear fit module in the commercial software Excel 2003; the cross-plot was drawn based on this result (as shown in figure 5). ...
Context 2
... figure 5, the abscissa represents the determination coefficient, the ordinate in the RD represents the response value of the deep resistivity curve, TH represents the response curve of the thorium content value, KTH represents the uranium gamma curve response value, CNL represents the neutron log response value, PE represents the value of the photoelectric absorption index log response curve, GR represents the gamma ray logging curve value, AC represents the wave slowness response curve, U represents the response curve of the uranium content value and DEN represents the density curve of the response value. It can be seen from figure 5 that the TOC and the density value have the biggest correlation. ...
Context 3
... figure 5, the abscissa represents the determination coefficient, the ordinate in the RD represents the response value of the deep resistivity curve, TH represents the response curve of the thorium content value, KTH represents the uranium gamma curve response value, CNL represents the neutron log response value, PE represents the value of the photoelectric absorption index log response curve, GR represents the gamma ray logging curve value, AC represents the wave slowness response curve, U represents the response curve of the uranium content value and DEN represents the density curve of the response value. It can be seen from figure 5 that the TOC and the density value have the biggest correlation. This is because the density of kerogen (a component of TOC) is much smaller than that of other lithology. ...
Context 4
... order to compare the models conveniently, the measure- ment of the TOC was carried out on 132 rock samples from the Longmaxi shale gas reservoir of the Jiaoshiba area in the Sichuan Basin (the first large shale gas field in China). With the sample points of the abnormal response value removed, the simple linear correlation of the log response and the TOC was analyzed using a crossplot single linear fit module in the commercial software Excel 2003; the cross-plot was drawn based on this result (as shown in figure 5). ...
Context 5
... figure 5, the abscissa represents the determination coefficient, the ordinate in the RD represents the response value of the deep resistivity curve, TH represents the response curve of the thorium content value, KTH represents the ura- nium gamma curve response value, CNL represents the neutron log response value, PE represents the value of the photoelectric absorption index log response curve, GR represents the gamma ray logging curve value, AC represents the wave slowness response curve, U represents the response curve of the uranium content value and DEN represents the density curve of the response value. It can be seen from figure 5 that the TOC and the density value have the biggest correlation. ...
Context 6
... figure 5, the abscissa represents the determination coefficient, the ordinate in the RD represents the response value of the deep resistivity curve, TH represents the response curve of the thorium content value, KTH represents the ura- nium gamma curve response value, CNL represents the neutron log response value, PE represents the value of the photoelectric absorption index log response curve, GR represents the gamma ray logging curve value, AC represents the wave slowness response curve, U represents the response curve of the uranium content value and DEN represents the density curve of the response value. It can be seen from figure 5 that the TOC and the density value have the biggest correlation. This is because the density of kerogen (a comp- onent of TOC) is much smaller than that of other lithology. ...

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Citations

... Numerous studies have made efforts to make connections between the geochemical parameters and well log responses (Fertl and Rieke 1980;Passey et al. 1990;Huang and Williamson 1996;Bordenave and Huc 1995;Alizadeh et al. 2012b;Sfidari et al. 2012;Mahmoud et al. 2017). Recent investigations are adopted as useful methods for the evaluation of the nonlinear relationship between TOC and well logs (Lewis et al. 2004;Kadkhodaie-ilkhchiy et al. 2009;Tan et al. 2015;Alizadeh et al. 2018;Bolandi et al. 2017;Zhu et al. 2018). According to the prior studies of the complicated and nonlinear relationships between TOC and well logs, an artificial neural network (ANN) is more applicable and advanced to evaluate TOC values. ...
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... Hydrocarbon Generation. TOC and S1+S2 were usually applied to evaluate hydrocarbon generation potential [40,41]. The bulk rock-normalized TOC and S1+S2 for bulk rock and residue after acidolysis indicate that acid treatment leads to hydrocarbon generable organic fraction loss, suggesting that conventional acid-treatment TOC measurements may underestimate the hydrocarbon generation potential. ...
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It has been acknowledged that carbonate was identified as the source rocks of a series of oil-gas fields worldwide. For evaluating the carbonate source rocks, total organic carbon (TOC) contents act as an important indicator. However, the acid solution, which has been generated during conventional TOC measurements, contain organic matters. Hence, the released organic matters in acid solution during carbonate decomposition may lead to underestimate the hydorcarbon generation potential. In this study, rock-eval pyrolysis technique was applied to bulk rock and residue after acid treatment. Meanwhile, the organic matters in acid solution were measured by Gas Chromatography-Mass Spectrometer (GC-MS) to investigate the geochemical characteristics. In addition, the hydrocarbon generation and alteration of TOC contents of released organic matters by acid treatment were studied by hydrous pyrolysis experiments. The results show that the acid solution contains organic compounds, including n-alkanes, saturated fatty acids and fatty acid methyl esters. Meanwhile, total organic carbon (TOC) contents and hydrocarbon generation potential (S1+S2) significantly decrease for bulk rocks after acid treatment in low maturity samples. Moreover, organic CO2 (S3) decreased after treating of acid, revealing that acidolysis process can affect and release organic matters containing oxygen-bearing functional groups. The S1, S2, S3, and TOC loss are positive correlation with the proportion of rock loss during acidolysis, indicating that the organic matters in acid solution are associated with carbonate minerals. The organic fractions may exist as adsorption state on the surface of carbonate minerals and (or) exist as organic acid salts. Moreover, the thermal simulation experiments reveal that the organic matter in acid solution, which is not recovered by the conventional measurement approach, could contribute to hydrocarbon generation.