Systems and methods for sensing and predicting the maturity of source rocks
A source rock and maturity technology, applied in the direction of reasoning methods, chemical property prediction, measurement devices, etc., can solve problems such as reducing fluid mobility, expensive production challenges, reducing the net value of final production products, etc., to achieve spatially accurate and timely results
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example 1
[0090] The source rock database contains measurements of various characteristics of source rock samples. For example, without limitation, a source rock database contains parameters (e.g., location and depth) associated with various source rock samples, as well as their Parameters (eg S1, S2, Tmax, HI, Oxygen Index (OI), Yield Index (PI), TOC, %Ro-Tmax and HI-%Ro). The source rock database may also contain FTIR data (eg, raw and preprocessed data, FTIR imaging data, and FTIR data of extracted samples), and elemental composition data (including individual mineral maps and mineral distributions for source rock samples). The source rock database also contains spectroscopic measurements and images, confocal fluorescence images, X-ray fluorescence images, ESR measurements, terahertz images and other data. The various methods used to obtain these metrics and examples of the data contained in the database are provided below.
[0091] In the wave number band 500-4000cm -1 FTIR spec...
example 2
[0106] The following examples are methods for selecting and optimizing sensing bands. The input is usually from curated primary rock databases. Sensing bands are selected and optimized using specific target attributes, such as a specific source rock maturity range or a specific organic facies distribution. Bands are selected to provide the most information for the selected target attribute, or to maximize differences in the target source rock sample. Band selection / optimization can be achieved by feature ranking and may also be constrained by the feasibility of sensor design and deployment.
[0107] In this example of sensing band optimization, the bands were chosen to differentiate clay from kerogen at different maturity levels. Apply a feature selection algorithm to calculate the weight of each frequency / wavenumber point. Figure 18 Alignment of weights representing grading features from FTIR spectroscopic measurements to spectral wavenumber bands to distinguish various c...
example 3
[0109] The following example is a method for clustering source rock samples by hierarchical clustering. The samples are divided into groups, where the source rock samples are similar to each other within each group but differ between groups. Maturity-specific signatures and cluster structures were derived to identify associated wavenumber bands and representative spectra. Figure 19A and Figure 19B is a representation of cluster plots from FTIR spectra of different samples projected on the selected wavenumber axis. Clustering is done in a high-dimensional space defined by wavenumber bands. Figure 19A shows the spectral wavenumber 1490.9cm using -1 (x-axis) and 2806.6cm -1 (y-axis) clustering results. Figure 19B Shown in terms of two different spectral wavenumber positions (3697 cm for the x-axis -1 , and for the y-axis is 2862.5cm -1 ) have the same clustering results. When projected in these two different coordinate systems, the same clustering result will have a d...
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