From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #8675 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 Thursday, March 17 2022 Volume 14 : Number 8675 Today's Subjects: ----------------- 50% OFF sale The best translator ever! ["Translator" Subject: 50% OFF sale The best translator ever! 50% OFF sale The best translator ever! http://thyrotor.buzz/TTYJq_dK8YzSemCezB0lFNwSgSRSBANkT8BVH9Txdl9RAdIMIw http://thyrotor.buzz/7W5zEaw9R6XFASAGUSe0nE09_jeKljf4DnZuKnXBtx37abTpew on occurs in clay during its formation, when lower-valence cations substitute for higher-valence cations in the crystal structure. Substitutions in the outermost layers are more effective than for the innermost layers, as the electric charge strength drops off as the square of the distance. The net result is oxygen atoms with net negative charge and the ability to attract cations. Edge-of-clay oxygen atoms are not in balance ionically as the tetrahedral and octahedral structures are incomplete. Hydroxyls may substitute for oxygens of the silica layers, a process called hydroxylation. When the hydrogens of the clay hydroxyls are ionised into solution, they leave the oxygen with a negative charge (anionic clays). Hydrogens of humus hydroxyl groups may also be ionised into solution, leaving, similarly to clay, an oxygen with a negative charge. Cations held to the negatively charged colloids resist being washed downward by water and are out of reach of plant roots, thereby preserving the fertility of soils in areas of moderate rainfall and low temperatures. There is a hierarchy in the process of cation exchang ------------------------------ Date: Thu, 17 Mar 2022 09:24:23 -0400 From: "BloodStream" Subject: #1 reason youâre losing your hair... #1 reason youbre losing your hair... http://moneyfort.icu/2jTt9sGYtUoUNtqFg_QgHBXdzu7a7pf8sdNNuuYdKlmVUxpP http://moneyfort.icu/kSET_7hoaJQGhW9A54_FQysIDOSavJ0tqDpZ4MFJ9-AbuXTNqQ lates in the soil pore system. At extreme levels CO2 is toxic. This suggests a possible negative feedback control of soil CO2 concentration through its inhibitory effects on root and microbial respiration (also called 'soil respiration'). In addition, the soil voids are saturated with water vapour, at least until the point of maximal hygroscopicity, beyond which a vapour-pressure deficit occurs in the soil pore space. Adequate porosity is necessary, not just to allow the penetration of water, but also to allow gases to diffuse in and out. Movement of gases is by diffusion from high concentrations to lower, the diffusion coefficient decreasing with soil compaction. Oxygen from above atmosphere diffuses in the soil where it is consumed and levels of carbon dioxide in excess of above atmosphere diffuse out with other gases (including greenhouse gases) as well as water. Soil texture and structure strongly affect soil porosity and gas diffusion. It is the total pore space (porosity) of soil, not the pore size, and the degree of pore interconnection (or conversely pore sealing), together with water content, air turbulence and temperature, that determine the rate of diffusion of gases into and out of soil. Platy soil structure and soil compaction (low porosity) impede gas flow, and a deficiency of oxygen may encourage anaerobic bacteria to reduce (strip oxygen) from nitrate NO3 to the gases N2, N2O, and NO, which are then lost to the atmosphere, thereby depleting the soil of nitrogen, a detrimental process called denitrification. Aerated soil is also a net sink of methane (CH4) but a net producer of methane (a strong heat-absorbing greenhouse gas) when soils are depleted of oxygen and subject to elevated temperatures. Soil atmosphere is also the seat of emissions of volatiles ------------------------------ Date: Thu, 17 Mar 2022 07:58:49 -0400 From: "Turning Democrats" Subject: Liberals' Closet Skeletons Exposed Liberals' Closet Skeletons Exposed http://ketopure.biz/eAdpJLIXHlxW5TtdxPdyRhGofJtSC_1nCl33AgcCChe4lHQ http://ketopure.biz/i-rx868RNu-Cwz9QZEWordNd5uHTxiIRxzKTebqE0aX6riU what 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 from the rocks. Crevasse ------------------------------ Date: Thu, 17 Mar 2022 10:38:31 -0400 From: "Prosperity" Subject: Your Unique Money Code (add $ to your income) Your Unique Money Code (add $ to your income) http://moneyfort.icu/dzItgzEhkLLPvcxdOuvJQawpkOKfbyd_tybrchbhFFnsp1kIEg http://moneyfort.icu/wBhvXrG0siVl3dmn6_I6O6YP4hG8f70plx61ybbtg0dOkRuM-A n heraldry, a motto is often found below the shield in a banderole; this placement stems from the Middle Ages, in which the vast majority of nobles possessed a coat of arms and a motto. In the case of Scottish heraldry it is mandated to appear above the crest. Spanish coats of arms may display a motto in the bordure of the shield. In heraldic literature, the terms "rallying cry" respectively "battle banner" are also common, which date back to the battle cry, and is usually located above the coat of arms. In English heraldry mottos are not granted with armorial bearings, and may be adopted and changed at will. In Scottish heraldry, mottos can only be changed by re-matriculation, with the Lord Lyon King of Arms. Although unusual in England and perhaps outside English heraldic practice, there are some examples, such as in Belgium, of the particular appearance of the motto scroll and letters thereon being blazoned; a prominent example is the obverse of the Great Seal of the United States (which is a coat of arms and follows heral ------------------------------ Date: Thu, 17 Mar 2022 08:05:56 -0400 From: "LingoGet" Subject: Experts Stunned with this Crazy Method to Learn Languages Experts Stunned with this Crazy Method to Learn Languages http://longzila.co/kZZverDrk0vLygE9hP93TTVITtZiG-cDYCES_1PceJfcKQzf http://longzila.co/O_RkFwJcnN5KL3P0FksA57PBIWVqC01LaR4j4EkQo6HSnKSweQ 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 in a soil, which in turn affects the development of the soil, a complex feedback which is exemplified in the dynamics of banded vegetation patterns in semi-arid regions. Soils 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 nutri ------------------------------ Date: Wed, 16 Mar 2022 09:33:16 -0400 From: "Mellitox" Subject: Feed These Brain Cells And Escape Type 2 Diabetes Feed These Brain Cells And Escape Type 2 Diabetes http://melliitox.co/LK8kVn7fmQx-FcleL6XEsVhkUTXwnbPdwgulOFQw_hvR_vZOYA http://melliitox.co/g-DmQ6NcSvTZov8oNnEH2pecS3YpqfpGiuYlf4Gqa-nvODxHDw istinctive 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 from the ro ------------------------------ End of alt.music.moxy-fruvous digest V14 #8675 **********************************************