Important announcement

Dear visitor,

Please note that this OpenCourseWare platform will be replaced at the end of 2026 by a new platform (under the same url ocw.tudelft.nl).

Courses and their contents that are currently available the platform will partly be migrated. URL’s for this content will change and content might be unavailable for some time. In addition, some courses will not be available anymore.

If you are linking to specific courses on this platform (for instance for your students), please take timely measures to avoid problems with access. Possible actions are:

  • Download the materials to your local platform (laptop, server)
  • For educators only (including TU Delft lecturers): Contact us at ocw@tudelft.nl and inform us what course you are using in what context (institute, program, period of use, number of students). We will research (in collaboration with the authors of the course) and decide if we will migrate the course, and if yes, can supply you with a new url.

Thank you.

In the first part of the lecture, the carbon cycle is explained. First, the concepts of organic carbon, inorganic carbon and phytoplankton are explained since these are crucial for understanding the carbon cycle. After that the carbon cycle and moreover mass balances that go together with the carbon cycle are presented as well.

Next, the evolution of the atmosphere is discussed where the development of Flora and Fauna is explained by interpreting the partial pressure of several gases in the atmosphere. Also, the composition of different biomolecules and their abundance in different organisms is explained.

Next, preservation of organic matter is explained. It can be seen that source rocks are the main preservation zones, which indicates the low efficiency of the preservation process. The concepts of Total Organic Carbon (TOC) and kerogen as a content of that in source rocks are elucidated.

Lastly, the conversion of kerogen in source rocks to hydrocarbons like oil and natural gas are explained. The “van Krevelen” diagram is used to illustrate this. Several types of maturation indicators, used to evaluate potential source rocks, are discussed.

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