Real0ne -> RE: The gift of rising CO2 just keeps on giving (9/14/2017 12:24:13 AM)
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ORIGINAL: MasterJaguar01 quote:
ORIGINAL: DesideriScuri quote:
ORIGINAL: MasterJaguar01 quote:
ORIGINAL: Real0ne [sm=champ.gif] Bingo! Yahtze! You got it, plants dont get their nutrients from air, every farmer on the planet knows you have to either replenish the soil or rotate crops in a manner that self replenishes. Thats why Phds get a Phd so they can show us how fucking stupid they are with their half asses analysis in support of the latest Zio Jiz. Bingo! Yahtze! You TOTALLY misunderstand the issue. Where plants get their nutrients from is COMPLETELY irrelevant. The theory is: The increased photosynthesis, due to increased CO2, leads to more carbohydrates (e.g. glucose), and less nutrients that benefit humans. You are COMPLETELY misunderstanding, confusing, and conflating nutrients that plants need for THEIR health with nutrients which plants produce which benefit OUR health. See excerpt below: But as the zooplankton experiment showed, greater volume and better quality might not go hand-in-hand. In fact, they might be inversely linked. As best scientists can tell, this is what happens: Rising CO2 revs up photosynthesis, the process that helps plants transform sunlight to food. This makes plants grow, but it also leads to them pack in more carbohydrates like glucose at the expense of other nutrients that we depend on, like protein, iron and zinc. I don't think he missed the point. The greater photosynthesis rate doesn't mean that the uptake of minerals/nutrients from the soil is any different. Increasing the rate at which foliage or other plant matter grows without increasing nutrient uptake from the soil means the plant is going to have a lower density of those nutrients/minerals. For instance, you have to limit the amount of foliage and fruiting on a grape vine to match it's ability to get nutrients from the soil, or you'll have a poor harvest. This isn't rocket surgery. He most definitely DID miss the point. The article mentions nothing about uptake from the soil. Rather than my paraphrasing: Rising CO2 revs up photosynthesis, the process that helps plants transform sunlight to food. This makes plants grow, but it also leads to them pack in more carbohydrates like glucose at the expense of other nutrients that we depend on, like protein, iron and zinc. It's NOT a question of getting anything from the soil. (Hence the missed point) as usual more bs completely inconclusive political study like the rest of climate bs being pedaled. climate howlers forget there is much more to this than meets the eye, nutrient levels of plants can easily vary 20% from contry to country as a result of the soil they are grown in so whats the big trama LOL V. How Mineral Nutrients Are Depleted in US Soils. A. Crop Removal and Livestock Operations The practice of removing part or all of the crops grown from the soil accelerates the loss of nutrients from the soil. The cycling of nutrients from plant uptake and release is interrupted by crop removal. This loss, if not corrected by fertilization, must be made up by nutrient release from primary soil minerals and from soil organic matter. Heavy tillage of soils adds oxygen which accelerates the decomposition of soil organic matter and increases in the release of nutrient elements. In soils with high levels of native soil humus, this "mining" of soil nutrients can occur over decades with little sign of soil exhaustion. Eventually, the humus content drops low enough so that it cannot supply enough nutrients to feed the crop. Nitrogen is usually the first element that is affected by soil tilling. Since primary soil minerals are not reservoirs of nitrogen, fertilization with nitrogen or rotation with nitrogen fixing crops (legumes) becomes necessary early on to maintain production. In livestock operations the cycling of nutrients in the soil is also interrupted. Meat and dairy products are sold off-farm, so the organic material is not returned to the soil. In some areas large feedlots have replaced on-farm operations. Typically in large feedlots the manure is not returned to the farm. If the manure created is not returned to the farm, the nutrients contained are lost. B. Soil Erosion Soil erosion is particularly devastating on older, more highly weathered soils in the southeast U.S. since the supply of tiny nutrient-rich primary minerals is already limited. Erosion removes the soil organic matter where much of the soil's nutrient reserve exists. Soils that are low in organic matter, or have lost much of it through erosion exhausts the soil's native nitrogen supply quickly compared to soils unaffected by erosion or low organic matter. Erosion of soil organic matter not only causes nitrogen loss, but also loss of other nutrients, including sulfur and boron. Soil erosion is a problem on privately held lands and public lands alike. For decades, overgrazing on public lands has resulted in soil erosion, which is severe in many areas. This overgrazing plus erosion has reduced the incidence and tonnage of palatable forage species available to livestock. Thus the yield of nutrients from those soils to livestock via forage has been substantially reduced by erosion and overgrazing. Standards for allowable levels of soil erosion were set by the Soil Conservation Service at 3 - 5 tons/acre/year for most soils. Today, soil erosion in the U.S. is nearly twice that level, although declining due to the implementation of protective measures.[15][15] C. Increased Nutrient Demand by Higher Yielding Crops Advances in plant breeding and management expertise have resulted in crops with far higher yield potential. For example, corn yields of 50 bushels an acre were considered quite good in the 1930's. Since the 1960's, corn yields over 200 bushels an acre are not uncmmon on more productive soils. This greatly increased demand by the new crops on the nutrient resources of most soils cannot be sufficiently met by natural release from primary minerals and organic matter. Thus the deficiency of the rate of nutrients released by soils for these super crops is induced by the high yield crops' greatly increased demands on the soil. Usually, the ability of a soil's primary minerals to supply enough phosphorus and potassium becomes limited under high yield cropping because both elements are required in relatively large amounts by plants. Thus, those elements are usually applied as fertilizer salts in conventional farming systems, or as biomass or crushed rocks containing these elements in certified organic systems. Almost all fertilization regimes now require regular inputs of those elements due to the effects of high yield crops. D. Depletion of Nutrient Bases Creates Soil Acidity As cropping continues on mature soils, and as soils age in natural systems under leaching conditions, the soils slowly become acidic. As basic nutrient elements like potassium, calcium and magnesium are lost via leaching and crop removal, acidic elements are created or released from clay minerals. There are other sources of acidity in soils (nitrification of ammonium nitrogen), but the loss of nutrient bases, without sufficient replacement by release from primary minerals, eventually leads to acid soils. In almost all soils, the most abundant available nutrient element is calcium, followed by magnesium. When soils become acid, and those elements are lost, the application of crushed limestone is needed to neutralize the soil acidity, and replace the calcium and magnesium. Federal subsidies to farmers for the application of lime to acid soils was highly successful in the mid-twentieth century. The federal government has discontinued those subsidies and not all farmers have continued adding lime frequently enough to replace the calcium and magnesium removed by cropping and from acids created by nitrogen fertilizers. E. Development of Micronutrient Deficiencies through Long-Term Crop Removal The long-term, heavy demands of high-yielding crops on the nutrient supply by soil primary minerals and organic matters may show up as shortages of micronutrient elements (iron, manganese, zinc, copper, boron, nickel, molybdenum, etc.). Many soils are naturally low in available levels of one or more of these elements. But heavy crop demands over time may increase the severity of the deficiency, and begin to exhaust the soil's ability to supply sufficient quantities of other micronutrient elements. Such deficiencies, if mild, often do not show visible symptoms in the plants. A slight yield decline may or may not be noticed. Soil and plant tissue testing are needed to verify these mild deficiencies. Many farmers do not perform these micronutrient tests on plants and soils until the deficiencies become severe enough to be noticed. If micronutrient deficiencies are identified, soluble sources of those nutrients must be applied to the soil. Foliar applications of micronutrients[16][16] may provide temporary relief, but must be repeated at regular intervals unless the soil deficiencies are corrected. Additions of organic matter or humates (oxidized lignites) may provide organic acids that help speed the release of micronutrient elements from primary minerals, if the necessary primary minerals are present. F. Western Alkaline Soils Soils in the more arid regions of the western U.S. are irrigated to supply enough water to grow crops and to leach out salts that may exist in high levels in the soil. In some areas the irrigation water is high in salts so extra water must be applied to prevent salt buildup and leach out the excess salts. When this happens, some nutrient elements are also leached out with the water (nitrogen, potassium, boron, etc.). Those elements must eventually be replaced if soil primary mineral release of these elements cannot keep up with plant demand. However, sodium, bicarbonates and the natural hardness (calcium + magnesium) of much western irrigation water keeps the soil alkaline. That alkalinity, whether native or induced through irrigation, greatly reduces the solubility of mineral elements like phosporus, iron, manganese and zinc. Plants cannot absorb insoluble mineral elements. This type of chemically induced "deficiency" is corrected by a variety of strategies, including concentrating fertilizers in a band, foliar feeding micronutrients, soil acidification, growing adapted varieties of crops, increasing organic matter contents through biomass addition, and long rotations with forage crops. Again, sufficient management expertise is needed, or access to such expertise must be utilized, to maintain nutrient levels and balances. G. Over-Fertilization with Some Nutrient Elements can Create Deficiencies in the Supply of Other Nutrients. Soils are complex systems, and this fact holds true when considering the plant availability of mineral nutrient elements. Fertilization with highly soluble commercial sources of nutrients has an effect on the plant availability of other nutrients. For example, heavy fertilization with ammonium-N may reduce potassium availability. High levels of ammonium-N or magnesium can reduce calcium availability. However, when high amounts of macronutrients are applied, often micronutrient availability is adversely affected. High applications of nitrate-N may reduce iron availability. Long term phosphorus application will reduce zinc availability and, to a lesser extent, iron availability. Since most growers fertilize with macronutrients, and fewer test for or apply micronutrients, this form of induced micronutrient deficiency can be a significant problem in many soils. H. Livestock Grazing on Public Lands Public lands (Bureau of Land Management; Forest Service) have been leased by ranchers for grazing by livestock for nearly a century. Although the deposition of manure does return some mineral elements to the soils, the nutrients captured in the weight gain the animals accrue is removed. Fertilization of these public lands by the US Government and the lessors is not usually practiced. Thus this slow deficit in nutrient balance has been continuing for a long time.
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