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Harvest went well. Chopped them down. Hanging now with a gentle fan. Chopped a few lower branches to dry and smoke while waiting. Havent weighed anything yet. Will add weights to this week soon. A total of 14.3 oz.
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@Aegon
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i love this strains very much ใกล้จะตัดแล้ว
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@mheat
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The leaves are weird on some branches. Also have lits of gnats. How do I rid of them?
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Die kleine Prinzessin macht Ihrem Namen alle Ehre. Kommt raus, und bleibt nach einer Woche 2 cm klein. Mal was neues. Man könnte vermuten, das es evtl. an der mittlerweile alten Genetik liegt. Moderne Strains sind bei gleichen Bedingungen ein zigfaches größer. Wir werden sehen wie es weiter geht. 🙀
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Strain: Chill Out OG F4 Harvest Day 64 Flower Day: 113 from sprout Medium: Fox Farm Ocean Forest Light: Vivosun VS2000 at 100% VPD: 1.5 kPa Light Distance: 12 inches Watering: By hand, ~oz daily Nutrients: pH Perfect Advanced Nutrition Grow, Bloom, Micro 2 ml / L, 1 ml / L big bud 30 inches YIELD: 54 grams dry and trimmed. Pretty sticky. Piney and floral smell (girlfriend said smelt a little like Christmas)
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Servus Moin! Die F025 macht jetzt langsam richtig dicke Buds. Sie hat ein sehr süßen, limonischen oldschool Geruch. Mir gefällt dieser Geruch sehr. Zum Glück habe ich noch 4 Samen von ihr. Könnte ein Grow-again werden.
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buds have started to ripen up all over the plant now, I think its another week max then flush time for the first ladies 💦💚🤟
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@TTerpz
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Start of week 6!! One more week until flip All pits have been brought back up to ph range in the 6s
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Servus Moin! Die Super Lemon Haze hat richtig gut aufgeholt und sich super ausgebildet. Jetzt kann es ja in den Sommer gehen.
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Hey everyone :-) This week it smells more and more sweet and fruity in the whole room 😍. There is actually not much to report, everyone is now under 12/12 :-). This is the last grow that comes in the entire diary. From now on, each plant will be added to the diary 👍. I wish you all a lot of fun watching, stay healthy 🙏🏻 and let it grow 😎👌
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Not much to report this week so far. Slightly defoliated above the Scrog to allow more light penetration for the lower branches. Plants starting to stretch abit now but nothing to bad.
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Day 56-59 from seed. End of week 8. ( soaked in water before planting on March 7th) Great bud development over the past week. Starting to smell and really pouring on the THC. Last heavy feeding on day 58. Lowered my RH 35% (as low as it it can go, how low can ya goooo). Temp is 24c probably going to say right there until the end. Still all clear trichomes on the plants inspected with my microscope. Apologies for my pictures it’s impossible for me to take all my plants out of my tent when there this size so I won’t have full pictures of the plants until the final week I hope these do them some justice.
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Start of week 2. Everything seems to be ok. The bottom left and right seem to have taken the lead. I switched the two biggest plants into the center. And raised the pots off the ground to help with airflow and temps. Plants are doing good. Two centers are taking the lead. Using RO water. Currently watering when top two inches are dry.
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Week 10...The plants are looking good! Took out the microscope to look at the trichomes...Starting to get milky but still another week or two before the harvest! Started flushing the plant this week!
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End of Week 3 switched back to "Snoop's Premium Nutrients Radical Roots"
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first pic was april 25 second the 26 and about two day in between or so on the others up until today the may the 3rd last day of week 7 now i can say things are starting to look good 😌 thru picture of what it looks like under the bed in case anyone was curious.. one has slight light burn finally got passed me and didn’t give in aha till today aha (edit ) i forgot to mention pots are about 15 in and yea i measured from the floor every time old habits aha
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Seedling managing 93F 30%RH, around 20 DLI. Vpd is in the 3's. No I don't recommend. Signum Magnum. "A great sign appeared in the sky a woman clothed with the sun with the moon under her feet and on her head a crown of twelve stars. Sing ye to the Lord a new canticle: because He has done wonderful things. Glory to the Father, and to the Son, and to the Holy Spirit As it was in the beginning, and now, and ever shall be, world without end." The plant nutrient nitrogen exists in forms with both positive and negative charges. Ammonium (NH4+)(immobile in soil)(Cation) has a positive charge, while nitrate (NO3-) (highly mobile in soil)(Anion)has a negative charge. Nitrogen is unique among plant nutrients in that it can exist in both positively charged (ammonium, NH₄⁺) and negatively charged (nitrate, NO₃⁻) forms in the soil. This makes it a special nutrient. In that it is responsible for providing balance for reactionary trade offs when it comes to ph. Because ph itself in the medium will always slowly drift towards acidicity, such is nature. 80% of nitrogen should be nitrate and no more than 20% ammoniacal nitrogen. Ca, mg, and K are the big 3 cations related to soil composition, pH & base saturation. When nitrogen is in the form of ammonium, it can compete with calcium, magnesium, and potassium for absorption sites in the plant root. This competition can lead to a reduction in the uptake of these other essential nutrients. Nitrogen, particularly in its nitrate form (NO3-), can increase soil acidity, which can also affect the availability of calcium, magnesium, and potassium. The form of nitrogen applied (ammonium vs. nitrate) can influence its interactions with other nutrients. Ammonium nitrogen can have a more pronounced negative effect on the uptake of calcium, magnesium, and potassium compared to nitrate nitrogen. Common forms of ammonium nitrogen include ammonium ion (NH4+), urea, and ammonium compounds like ammonium nitrate, ammonium sulfate, and ammonium phosphate. Common forms of nitrate nitrogen include potassium nitrate (KNO3), sodium nitrate (NaNO3), calcium nitrate (Ca(NO3)2), and ammonium nitrate (NH4NO3). Phosphorus is an essential plant nutrient, and its availability in the soil is strongly linked to the presence of oxygen. Plants primarily absorb phosphorus as phosphate (PO4), and oxygen is a key component of this molecule. Furthermore, the availability of phosphorus in the soil can be impacted by factors like soil aeration and temperature, which in turn affect the oxygen supply to the roots. Phosphorus uptake in plants is most critical during the early stages of growth, particularly within the first few weeks of plant development. Young plants actively growing tissues have a high demand for phosphorus. They may absorb up to 75% of their total phosphorus requirements within the first few weeks of vegetative growth, with up to 51% of uptake happening overnight, primarily in the first few hours or early nightfall. ⑨Anaerobic root respiration, or respiration without oxygen, is detrimental to plants because it's less efficient and produces toxic byproducts, leading to reduced energy production, nutrient uptake issues, and ultimately, root damage and plant stress. ⑨Anaerobic respiration, unlike aerobic respiration, doesn't utilize oxygen as the final electron acceptor in the electron transport chain. This results in a significant drop in the amount of energy (ATP) produced, which is necessary for various plant functions, including growth, nutrient uptake, and maintenance of cellular processes. ⑨In the absence of oxygen, plants produce byproducts like ethanol and lactic acid during anaerobic fermentation. These byproducts can be toxic to the roots and inhibit their function, ⑨When oxygen is depleted in a medium, the pH tends to decrease (become more acidic) due to the production of metabolic byproducts. This is particularly relevant in biological systems where aerobic respiration relies on oxygen as the final electron acceptor. ⑨When oxygen is scarce, plants may switch to anaerobic respiration. This process produces carbon dioxide (CO2) as a byproduct. ⑨CO2 dissolves in water to form carbonic acid (H2CO3). This acid lowers the pH of the medium, making it more acidic. ⑨Anaerobic conditions can impair a plant's ability to regulate its internal pH, leading to a drop in cytoplasmic pH and potentially cellular acidosis. ⑨The change in pH can also affect the availability of certain nutrients to the plant, as pH influences the solubility of micronutrients like iron, manganese, zinc, copper, and boron. ⑨The lack of oxygen in the plant medium leads to a decrease in pH due to the production of carbon dioxide during anaerobic respiration and impaired pH regulation within the plant. In plant cells, cellular acidosis, a drop in the internal pH of the cytosol, is a significant stress response, particularly during conditions like flooding or hypoxia. This acidification can be triggered by a decrease in oxygen levels, leading to the production of metabolic byproducts like lactic acid and CO2. The plant's ability to tolerate and recover from these conditions depends on its cellular mechanisms to regulate pH and mitigate the effects of acidosis. When plants are subjected to low oxygen environments, such as those experienced during flooding, anaerobic metabolism, which produces lactic acid and ethanol, becomes the primary source of energy. This can lead to a build-up of these acidic metabolites in the cytosol, causing a drop in pH. OXYGEN Atomic oxygen (single oxygen atom, O) is the lightest form of oxygen, as it has the lowest mass of the oxygen molecules. Oxygen also exists as a diatomic molecule (O2) and an allotrope called ozone (O3), which have higher masses due to the number of oxygen atoms combined. Atomic Oxygen (O): This refers to a single oxygen atom, which is the most fundamental form of oxygen. Molecular Oxygen (O2): This is the common form of oxygen we breathe, consisting of two oxygen atoms bonded together. Ozone (O3): This is an allotrope of oxygen, meaning it's a different form of the same element, consisting of three oxygen atoms bonded together. Since atomic oxygen has the fewest oxygen atoms, it naturally has the lowest mass compared to O2 or O3. Ozone (O3) Lifespan: Ozone has a relatively long lifespan in the stratosphere, particularly at lower altitudes. For example, at 32 km in the middle latitudes during spring, ozone has a lifetime of about 2 months. Oxygen (O) Lifespan: Atomic oxygen, on the other hand, has a much shorter lifespan. At the same altitude, its lifetime is about 4/100ths of a second. Ozone-Oxygen Cycle: The ozone-oxygen cycle involves the rapid exchange between atomic oxygen (O) and ozone (O3). UV radiation can split molecular oxygen (O2) into atomic oxygen (O), which then reacts with O2 to form ozone (O3). Ozone can also be photolyzed by UV radiation, creating atomic oxygen again, which can then react with O3 to reform O2. Dominant Form: The partitioning of odd oxygen (Ox) between ozone and atomic oxygen favors ozone in the lower stratosphere. This means that a much larger proportion of odd oxygen exists as ozone than as atomic oxygen, especially in the lower stratosphere. Recombination: Atomic oxygen has a high energy and reactivity. When it encounters another oxygen atom, they can combine to form O2. This process releases energy, contributing to the heating of the atmosphere. Ozone Formation: Atomic oxygen can also react with molecular oxygen (O2) to form ozone (O3). Ozone plays a significant role in absorbing harmful UV radiation. Other Reactions: Atomic oxygen can react with various other molecules in the atmosphere, like nitrogen (N2), water (H2O), and carbon dioxide (CO2), forming different compounds. UV light below 240nm (peak 185nm) creates ozone (O₃) through a process called photolysis, where UV light breaks down dioxygen molecules (O₂) into single atomic oxygen atoms (O). These single oxygen atoms then react with other oxygen molecules to form ozone (O₃). Specifically, UV-C light with wavelengths shorter than 240 nm can cause this photolysis. UV light with wavelengths between 240-280 nm, (peak 254 nm) breaks down ozone (O₃) into dioxygen molecules (O₂) and atomic oxygen atoms (O). 280nm does not have the energy potential to break apart the stable bond of (O₂) into enough (O) to make (O₃) At ground level, atomic oxygen (single oxygen atoms) has a very short lifespan. This is because it's highly reactive and quickly combines with other molecules to form stable diatomic oxygen (O2) or other compounds. While the exact timeframe varies depending on the specific circumstances, its lifespan is typically measured in nanoseconds or picoseconds.