<resource xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://datacite.org/schema/kernel-4" xsi:schemaLocation="http://datacite.org/schema/kernel-4 http://schema.datacite.org/meta/kernel-4.3/metadata.xsd">
    <identifier identifierType="DOI">10.5880/GFZ.3.6.2021.002</identifier>
    <creators>
     <creator>
      <creatorName nameType="Personal">Gottschalk, Matthias</creatorName>
      <givenName>Matthias</givenName>
      <familyName>Gottschalk</familyName>
      <nameIdentifier nameIdentifierScheme="ORCID">0000-0003-0430-2666</nameIdentifier>
      <affiliation>GFZ German Research Centre for Geosciences, Potsdam, Germany</affiliation>
     </creator>
    </creators>
    <titles>
     <title>Evaluation of numerous J-, K-, L-, M-, and N-integrals used in perturbation theory: Integral raw data</title>
    </titles>
    <publisher>GFZ Data Services</publisher>
    <publicationYear>2021</publicationYear>
    <subjects>
     <subject>Monte-Carlo simulations</subject>
     <subject>Lennard-Jones fluid</subject>
     <subject>configurations</subject>
     <subject>pair-correlation functions</subject>
     <subject>triplet-correlation functions</subject>
     <subject>pair-integrals</subject>
     <subject>triplet-integrals</subject>
     <subject subjectScheme="NASA/GCMD Earth Science Keywords">EARTH SCIENCE SERVICES &gt; MODELS &gt; PHYSICAL/LABORATORY MODELS</subject>
    </subjects>
    <contributors>
     <contributor contributorType="ContactPerson">
      <contributorName>Gottschalk, Matthias</contributorName>
      <affiliation>GFZ German Research Centre for Geosciences, Potsdam, Germany</affiliation>
     </contributor>
     <contributor contributorType="ContactPerson">
      <contributorName>Gottschalk, Matthias</contributorName>
      <affiliation>GFZ German Research Centre for Geosciences, Potsdam, Germany</affiliation>
     </contributor>
    </contributors>
    <resourceType resourceTypeGeneral="Dataset">Dataset</resourceType>
    <relatedIdentifiers>
     <relatedIdentifier relatedIdentifierType="DOI" relationType="IsSupplementTo">10.1080/00268976.2021.2000652</relatedIdentifier>
     <relatedIdentifier relatedIdentifierType="DOI" relationType="Cites">10.1063/1.5119761</relatedIdentifier>
     <relatedIdentifier relatedIdentifierType="DOI" relationType="Cites">10.1063/5.0048450</relatedIdentifier>
     <relatedIdentifier relatedIdentifierType="DOI" relationType="Cites">10.5880/GFZ.3.6.2021.001</relatedIdentifier>
    </relatedIdentifiers>
    <sizes/>
    <formats/>
    <rightsList>
     <rights rightsURI="http://creativecommons.org/licenses/by/4.0/">CC BY 4.0</rights>
    </rightsList>
    <descriptions>
     <description descriptionType="Abstract">Following Barker, Pople and Gubbins &amp; Gray, the u-expansion of the  perturbation theory, used for developing equations of state for fluids, requires sets of J-, K-, L-, M-, and N-integrals as a function of rho* and T*. These integrals are calculated here from pair and triplet correlation functions, which were derived in a previous communication, using particle configurations from extensive Monte-Carlo simulations of a Lennard-Jones fluid.       <br/>
      <br/>
The pair and triplet correlation functions are based on 27615 state points covering a rho*-T*  space from  0.002-1.41 and 0.45-25 in reduced variables, respectively, which is also the range of the calculated integrals. Quadruplet correlation functions, required by the M- and N-integrals, were calculated using the trans-superposition approximation, using pair and triplet correlation functions. Here the unfitted raw data of 597 J-, 90 K-, 256 L-, 4M-, and 4N-integrals are reported. The number of available  values at different rho*-T* state points are 27615 for the J-integrals, and in the range of  6999-7053, 6789-7055, 6440-6587, 6544-6751 for the  K-, L-, M-, andN-integrals, respectively.      <br/>
     </description>
    </descriptions>
   </resource>