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Very cool, thank you. Any chance you could make a PR for this? I have very limited time - down to an hour per week - to work on this so would like to get some help. |
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After some further testing, I believe you can leave everything as it is and just improve the documentation with something like this: Max bucket size reccomanded based on type of soil: The above is reccomanded based on the following: Determine Soil Water Holding Capacity: Understand the available water capacity (AWC) of your soil. For loam soil, this is typically 150-200 mm/meter. To avoid overwatering and encourage deep rooting, water deeply but infrequently. Multiplier reccomanded based on grass type: Cool-season grasses = 0.8 Also I would reccomand to water based on an automation that will be triggered and check the following conditions: Trigger: every day at 5am |
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This is very interesting. Thank you @acarlo79 Does this only apply to grass? I am using smart watering to water a tropical garden with a range of different plants - not grass. |
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Good day! But I think that the approach to the "bucket" needs to be radically changed! But when we work with a bucket in the range of both "-" and "+", it turns out that the maintenance works correctly only if the rains do not overflow the bucket more than 0. Let's look at an example: First step - irrigation until the moisture saturation level is 100%, the bucket = 0. If was no rain for a period of 4 days, then everything will work: the moisture will be taken away exactly as much as the smart watering calculates: 3mm * 4 days = 12mm But if the next day after watering there was a 10mm rainfall. The calculation will not work correctly: Irrigation will add 2mm of precipitation to make the bucket 0. After some time we will get a moisture saturation balance at the level of 0%-50%. Therefore, I propose to remove such a parameter as Maximum bucket and make a new parameter moisture capacity. Now I'm implementing this method with triggers, but if it's built-in, it will be much more convenient. Thank you for your attention. Translated via Google, so if the idea is not very clear, write to me. |
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The calculation can be affected by the type of grass. Different types of grass have different water requirements, which are accounted for by the crop coefficient (Kc). The crop coefficient varies depending on the type of grass and its growth stage. This coefficient adjusts the reference evapotranspiration (ET0) to reflect the actual water needs of the grass.
Understanding Crop Coefficient (Kc)
Cool-season grasses (e.g., fescue, bluegrass):
Typically have a higher Kc value, often ranging from 0.7 to 0.9 during their peak growing season.
Warm-season grasses (e.g., Bermuda, zoysia):
Generally have a lower Kc value, usually ranging from 0.6 to 0.8 during their peak growing season.
Adjusting the Calculation
To account for the grass type, we need to adjust the ET0 with the appropriate Kc value.
Daily ETc (Crop Evapotranspiration):
ETc = ET0 × Kc
Calculate the effective water requirement:
Adjusted Daily ET = 3 mm/day × Kc
Example Calculations
Cool-season Grass (Kc = 0.8)
Adjusted Daily ET:
ETc = 3 mm/day × 0.8 = 2.4 mm/day
We should take into consideration also the type of soil:
Determine Soil Water Holding Capacity:
Understand the available water capacity (AWC) of your soil. For loam soil, this is typically 150-200 mm/meter.
Calculate how much water your soil can hold in the root zone of your grass (usually 15-30 cm deep).
Example: For a 30 cm root zone in loam soil with 200 mm/m AWC: 200 mm/m * 0.3 m = 60 mm.
To avoid overwatering and encourage deep rooting, water deeply but infrequently.
Determine the allowable depletion level. Often, watering is done when 50% of the available water has been used.
Example: If the AWC in the root zone is 60 mm, you would water when 30 mm has been depleted (50%).
Look at this example:
Steps to Determine Watering Needs:
Evapotranspiration Rate (ET):
Daily ET = 3 mm/day.
Total Rainfall:
Rainfall over 2 days = 100 mm.
Soil Water Holding Capacity:
Clay soil typically has an available water capacity (AWC) of about 200 mm/meter.
Root Zone Depth:
Assuming the root zone depth for a lawn is 30 cm (0.3 meters).
Calculate the Available Water in the Root Zone:
AWC for clay soil in the root zone = 200 mm/meter × 0.3 meters = 60 mm.
Consider Effective Rainfall:
Rainfall received = 100 mm.
Since the soil's AWC is 60 mm in the root zone, any additional water will likely lead to runoff or deep percolation. Therefore, effectively, the soil will only use up to its capacity of 60 mm.
Calculate Depletion Rate:
Daily ET = 3 mm/day.
Days until the soil moisture is depleted = Available water / Daily ET = 60 mm / 3 mm/day = 20 days.
However, considering the rainfall:
Adjust for the Rainfall:
Rainfall far exceeds the soil's AWC. We consider only the 60 mm that the soil can effectively utilize.
Days provided by effective rainfall: 60 mm / 3 mm/day = 20 days.
Total Days Without Watering:
With effective use of rainfall and the high daily ET, you can go up to 20 days without watering, considering that the soil's water holding capacity is the limiting factor, not the total rainfall.
Considering Grass Type (Cool-season vs. Warm-season)
Cool-season Grass (Kc = 0.8)
Adjusted Daily ET:
ETc = 3 mm/day × 0.8 = 2.4 mm/day.
Effective Rainfall Contribution:
Total AWC used: 60 mm (limited by soil capacity).
Days provided by effective rainfall: 60 mm / 2.4 mm/day ≈ 25 days.
Warm-season Grass (Kc = 0.6)
Adjusted Daily ET:
ETc = 3 mm/day × 0.6 = 1.8 mm/day.
Effective Rainfall Contribution:
Total AWC used: 60 mm (limited by soil capacity).
Days provided by effective rainfall: 60 mm / 1.8 mm/day ≈ 33 days.
Conclusion
For cool-season grass (Kc = 0.8), you can go approximately 25 days without watering after 100 mm of rainfall, considering the soil's water holding capacity.
For warm-season grass (Kc = 0.6), you can go approximately 33 days without watering after 100 mm of rainfall, considering the soil's water holding capacity.
These calculations assume optimal conditions where all rainfall is effectively utilized and there is no additional water loss due to runoff or deep percolation.
So, to summarize, I would:
I think such options will further enahnce this tool.
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