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  2. Scientists explore how to improve crop yields - on Mars - AOL

    www.aol.com/news/scientists-explore-improve-crop...

    The crops were grown in simulated Martian regolith - soil with no organic matter - developed by NASA researchers that is a near-perfect physical and chemical match to real Martian soil.

  3. Crop rotation - Wikipedia

    en.wikipedia.org/wiki/Crop_rotation

    The formation of soil aggregates is important for erosion control, as they are better able to resist raindrop impact, and water erosion. Soil aggregates also reduce wind erosion, because they are larger particles, and are more resistant to abrasion through tillage practices. [32] The effect of crop rotation on erosion control varies by climate.

  4. BBCH-scale (solaneous fruit) - Wikipedia

    en.wikipedia.org/wiki/BBCH-scale_(solaneous_fruit)

    1 For tomatoes with determinate stem growth, paprika and aubergines. In tomatoes with indeterminate stem growth and only one sympodial branch at the corresponding axis, the apical side shoot formation occurs concurrently with the emergence of the inflorescence (Principal growth stage 5), so that the coding within principal growth stage 2 is not necessary

  5. Tomato grafting - Wikipedia

    en.wikipedia.org/wiki/Tomato_grafting

    Tomato grafting is a horticulture technique that has been utilized in Asia and Europe for greenhouse and high tunnel production and is gaining popularity in the United States. [1] Typically, stock or rootstock are selected for their ability to resist infection by certain soilborne pathogens or their ability to increase vigor and fruit yield.

  6. Important facts about North Texas soils and how to prepare ...

    www.aol.com/important-facts-north-texas-soils...

    The perfect soil should be 50% solid matter, 25% water, and 25% pore space (air/oxygen). After a heavy rain or irrigation, the pore space will fill up with water and the soil would become 50/50 ...

  7. Soil fertility - Wikipedia

    en.wikipedia.org/wiki/Soil_fertility

    Soil scientists use the capital letters O, A, B, C, and E to identify the master horizons, and lowercase letters for distinctions of these horizons. Most soils have three major horizons—the surface horizon (A), the subsoil (B), and the substratum (C). Some soils have an organic horizon (O) on the surface, but this horizon can also be buried.

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