From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #9170 Reply-To: ammf@fruvous.com Sender: owner-ammf-digest@smoe.org Errors-To: owner-ammf-digest@smoe.org Precedence: bulk alt.music.moxy-fruvous digest Wednesday, June 22 2022 Volume 14 : Number 9170 Today's Subjects: ----------------- Your free 21 keto recipes ["Keto Recipe" Subject: Your free 21 keto recipes Your free 21 keto recipes http://naturallywork.za.com/FQSmslRcXzLZupbvROk4MuSPA5c2uuQqTYmGufpRGbRqgd7WTA http://naturallywork.za.com/0Bi2KoKfA19lDUF_tdg9TV1Y8Rhp62Dn9L4jVVmLzPI5cvUl aid to be formed when organic matter has accumulated and colloids are washed downward, leaving deposits of clay, humus, iron oxide, carbonate, and gypsum, producing a distinct layer called the B horizon. This is a somewhat arbitrary definition as mixtures of sand, silt, clay and humus will support biological and agricultural activity before that time. These constituents are moved from one level to another by water and animal activity. As a result, layers (horizons) form in the soil profile. The alteration and movement of materials within a soil causes the formation of distinctive soil horizons. However, more recent definitions of soil embrace soils without any organic matter, such as those regoliths that formed on Mars and analogous conditions in planet Earth deserts. An example of the development of a soil would begin with the weathering of lava flow bedrock, which would produce the purely mineral-based parent material from which the soil texture forms. Soil development would proceed most rapidly from bare rock of recent flows in a warm climate, under heavy and frequent rainfall. Under such conditions, plants (in a first stage nitrogen-fixing lichens and cyanobacteria then epilithic higher plants) become established very quickly on basaltic lava, even though there is very little organic material. Basaltic minerals commonly weather relatively quickly, according to the Goldich dissolution series. The plants are supported by the porous rock as it is filled with nutrient-bearing water that carries minerals dissolved ------------------------------ Date: Wed, 22 Jun 2022 07:13:36 -0400 From: "New York Bagel Delivery" Subject: Do you LOVE a good bagel? Do you LOVE a good bagel? http://elephal.ru.com/hPY__mhMomgaQxH7TaLkBNKxzfk6AjIJKV87CdtCnc_cnYE-9A http://elephal.ru.com/kIfty7Ju-50f0yncPN7QMS97mz6_UPaKE1V6fWmETeEhOsBMsQ largely confined to the solum, and is generally more prominent in the A horizon. It has been suggested that the pedon, a column of soil extending vertically from the surface to the underlying parent material and large enough to show the characteristics of all its horizons, could be subdivided in the humipedon (the living part, where most soil organisms are dwelling, corresponding to the humus form), the copedon (in intermediary position, where most weathering of minerals takes place) and the lithopedon (in contact with the subsoil). The soil texture is determined by the relative proportions of the individual particles of sand, silt, and clay that make up the soil. The interaction of the individual mineral particles with organic matter, water, gases via biotic and abiotic processes causes those particles to flocculate (stick together) to form aggregates or peds. Where these aggregates can be identified, a soil can be said to be developed, and can be described further in terms of color, porosity, consistency, reaction (acidity), etc. Water is a critical agent in soil development due to its involvement in the dissolution, precipitation, erosion, transport, and deposition of the materials of which a soil is composed. The mixture of water and dissolved or suspended materials that occupy the soil pore space is called the soil solution. Since soil water is never pure water, but contains hundreds of dissolved organic and mineral substances, it may be more accurately called the soil solution. Water is central to the dissolution, precipitation and leaching of minerals from the soil profile. Finally, water affects the type of vegetation that grows ------------------------------ Date: Wed, 22 Jun 2022 06:51:41 -0400 From: "Home Depot Survey" Subject: Get all the lawn care gear you need! Get all the lawn care gear you need! http://chargeo.za.com/3TNMTI7xQg4GJ67TehHE57Xr8aTaHVlYQQCF9Ni0o7VcAnAF4Q http://chargeo.za.com/LObs6XOlZVbKSS4ci_zpCT08k9T_l63w367GY4kiLU3irgEV5A a major component of the Earth's ecosystem. The world's ecosystems are impacted in far-reaching ways by the processes carried out in the soil, with effects ranging from ozone depletion and global warming to rainforest destruction and water pollution. With respect to Earth's carbon cycle, soil acts as an important carbon reservoir, and it is potentially one of the most reactive to human disturbance and climate change. As the planet warms, it has been predicted that soils will add carbon dioxide to the atmosphere due to increased biological activity at higher temperatures, a positive feedback (amplification). This prediction has, however, been questioned on consideration of more recent knowledge on soil carbon turnover. Soil acts as an engineering medium, a habitat for soil organisms, a recycling system for nutrients and organic wastes, a regulator of water quality, a modifier of atmospheric composition, and a medium for plant growth, making it a critically important provider of ecosystem services. Since soil has a tremendous range of available niches and habitats, it contains a prominent part of the Earth's genetic diversity. A gram of soil can contain billions of organisms, belonging to thousands of species, mostly microbial and largely still unexplored. Soil has a mean prokaryotic density of roughly 108 organisms per gram, whereas the ocean has no more than 107 prokaryotic organisms per milliliter (gram) of seawater. Organic carbon held in soil is eventually returned to the atmosphere through the process of respiration carried out by heterotrophic organisms, but a substantial part is retained in the soil in the form of soil organic matter; t ------------------------------ Date: Wed, 22 Jun 2022 08:04:29 -0400 From: "Nutroxyn" Subject: Is Your Partner Really Tired In The Bedroom Is Your Partner Really Tired In The Bedroom http://consulto.za.com/lRjDsu5KW1sjQFOkS7CUXvtO-YCWH4AH15_nYVRo80w5Vv1LvA http://consulto.za.com/5i9fRzy35du0OnL6vo9R2N2iI7qLzpjZoZ-P2vLc--CDtUQixw s supply plants with nutrients, most of which are held in place by particles of clay and organic matter (colloids) The nutrients may be adsorbed on clay mineral surfaces, bound within clay minerals (absorbed), or bound within organic compounds as part of the living organisms or dead soil organic matter. These bound nutrients interact with soil water to buffer the soil solution composition (attenuate changes in the soil solution) as soils wet up or dry out, as plants take up nutrients, as salts are leached, or as acids or alkalis are added. Plant nutrient availability is affected by soil pH, which is a measure of the hydrogen ion activity in the soil solution. Soil pH is a function of many soil forming factors, and is generally lower (more acid) where weathering is more advanced. Most plant nutrients, with the exception of nitrogen, originate from the minerals that make up the soil parent material. Some nitrogen originates from rain as dilute nitric acid and ammonia, but most of the nitrogen is available in soils as a result of nitrogen fixation by bacteria. Once in the soil-plant system, most nutrients are recycled through living organisms, plant and microbial residues (soil organic matter), mineral-bound forms, and the soil solution. Both living soil organisms (microbes, animals and plant roots) and soil organic matter are of critical importance to this recycling, and thereby to soil formatio ------------------------------ Date: Wed, 22 Jun 2022 06:19:50 -0400 From: "Good News" Subject: BONUS: $90 PFIZER Gift Card Opportunity BONUS: $90 PFIZER Gift Card Opportunity http://elephal.ru.com/h_Os2T9bmIuZ1fwQri0hLWgnA9JLC18PGo-mn9oV4XnBAQpuVQ http://elephal.ru.com/JbtDnoZ-cX9LdYdU8g4VVpDNDTGGJaIzsUa7OIJeRR0onM6ykQ largely confined to the solum, and is generally more prominent in the A horizon. It has been suggested that the pedon, a column of soil extending vertically from the surface to the underlying parent material and large enough to show the characteristics of all its horizons, could be subdivided in the humipedon (the living part, where most soil organisms are dwelling, corresponding to the humus form), the copedon (in intermediary position, where most weathering of minerals takes place) and the lithopedon (in contact with the subsoil). The soil texture is determined by the relative proportions of the individual particles of sand, silt, and clay that make up the soil. The interaction of the individual mineral particles with organic matter, water, gases via biotic and abiotic processes causes those particles to flocculate (stick together) to form aggregates or peds. Where these aggregates can be identified, a soil can be said to be developed, and can be described further in terms of color, porosity, consistency, reaction (acidity), etc. Water is a critical agent in soil development due to its involvement in the dissolution, precipitation, erosion, transport, and deposition of the materials of which a soil is composed. The mixture of water and dissolved or suspended materials that occupy the soil pore space is called the soil solution. Since soil water is never pure water, but contains hundreds of dissolved organic and mineral substances, it may be more accurately called the soil solution. Water is central to the dissolution, precipitation and leaching of minerals from the soil profile. Finally, water affects the type of vegetation that grows ------------------------------ Date: Mon, 20 Jun 2022 07:23:07 -0400 From: "Forget Advil" Subject: Drops of this liquid eases pain on contact Drops of this liquid eases pain on contact http://spectators.za.com/aglCG_MpMuVPtLxyNuB7C3X7G5CEwnxoCTi6qsIVky6uItCCJA http://spectators.za.com/tGGYfHNuB7PZB8yKcMpTggIFYXKiuKXSzfV2rV_v3FGq4zLk5A he UNCIP appointed its successor, Sir Owen Dixon, to implement demilitarisation prior to a statewide plebiscite on the basis of General McNaughton's scheme, and to recommend solutions to the two governments. Dixon's efforts for a statewide plebiscite came to naught due to India's constant rejection of the various alternative demilitarisation proposals, for which Dixon rebuked India harshly. Dixon then offered an alternative proposal, widely known as the Dixon plan. Dixon did not view the state of Jammu and Kashmir as one homogeneous unit and therefore proposed that a plebiscite be limited to the Valley. Dixon agreed that people in Jammu and Ladakh were clearly in favour of India; equally clearly, those in Azad Kashmir and the Northern Areas wanted to be part of Pakistan. This left the Kashmir Valley and 'perhaps some adjacent country' around Muzaffarabad in uncertain political terrain. Pa ------------------------------ End of alt.music.moxy-fruvous digest V14 #9170 **********************************************