Open ramonawalls opened 6 years ago
Geologists make observations on parts of a rock sample, with specific intentions related to the properties of the sample as a whole. E.g. some mineral grain with the sample may be useful for dating, or inferring the pressure of formation of the assemblage. Is this different?
Yes.
On Sat, Sep 29, 2018 at 1:42 AM Simon Cox notifications@github.com wrote:
Geologists make observations on parts of a rock sample, with specific intentions related to the properties of the sample as a whole. E.g. some mineral grain with the sample may be useful for dating, or inferring the pressure of formation of the assemblage. Is this different?
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I think it is pretty similar. In the PPO example, we are trying to infer presence or absence, which requires some specific axioms, but the overall concept of inferring a quality of the whole based on the quality of a sample is the same, and worth considering.
This is an issue for the PPO (but unfortunately not on github), which needs to make inferences about the presence or absence of structures on a whole plant based on an observation of a plant part, either from a herbarium specimen or from an image of a plant part. However, I think the logic is needed more broadly and should be included in BCO.
PPO has addressed this issue by creating a class called "portion of plant", which is a proper part of a plant or "derived" from a proper part of a plant (the actual relations are not yet specified, because they don't exist in RO yet). PPO logic infers that is a structure is present on a part of a plant, it must have been present on the whole plant. If a structure is absent from the plant part, you cannot make an inference about its presence on the whole plant.
I suggest that BCO create upper terms with a similar design pattern that could be used in PPO or for other organisms.