Dear colleagues,

basically we intend to correlate lab measurements of soil stability (for details see below) with in situ measurements of soil stability. As in situ measurements we already have:

  • soil moisture (FDR probe)
  • depth of the skid trail (laser)
  • shear strength (shear vane tester)
  • penetration resistance (hand penetrometer)
  • oxygen diffusion rate (ODR meter)
  • saturated hydraulic conductivity, ks (hood-infiltrometer)
  • These methods are not all really simple and fast. So that's the point where I need your creative ideas.

    My question to YOU: What other simple field measurements could possibly be correlated to soil stability and/or function?

    It could also be something weird, or crazy, something I would not think of in first instance (e.g. sth related to electricity)

    Thanks a lot for your feedback,

    Malte

    Background of the question:

    Lab measurements, undertaken with samples from the field: pre-consolidation stress and cyclic compressibility, shear parameters, Atterberg limits, saturated hydraulic conductivity, air permeability, texture, water retention curve.

    Explanation of the project:

    My collegues an me want to assess the impact of heavy forestry machines (29t forwarder) on the stability and function of a loess soil (stagnosol). The trafficking experiments will be conducted on already existing skid trails in a spruce forrest. Different machine configurations (tyres, different kind of belts) will be compared with each other. For each machine configuration different trafficking frequencies and slope inclinations will be simulated.

    Laboratory experiments are, as the name already says, very laborous and expensive. Therefore we want to try to correlate the results from the lab to results from the field measurements. WIth the resulting pedotransfer functions it might be possible to derive the parameters from the lab measurements just from simple field measurements, so that in future the laboratory measurements could be skipped. With these field measurements large areas of forest soils could be covered rather easily and hence could be used to create maps of loess soil stability. These maps could serve the rangers as a decision guidance for a soil conserving wood harvest.

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