From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #9171 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, June 23 2022 Volume 14 : Number 9171 Today's Subjects: ----------------- Do THIS habit every morning or youâll NEVER lose weight ["Slow metabolism] Triggered by these 3 common fruits? ["Dangerous Hormones" ] Your Family Is In Serious Danger (leaked report) ["Every Disaster Claims"] Ray-Ban Sunglasses Up To 90% Off!Top Quality Low Cost! Shop Online Now! [] ---------------------------------------------------------------------- Date: Wed, 22 Jun 2022 10:50:51 -0400 From: "Slow metabolism" Subject: Do THIS habit every morning or youâll NEVER lose weight Do THIS habit every morning or youbll NEVER lose weight http://counselo.za.com/cSwuWEonOzB7e2EAFQ33oGn3navRVDotMfb2DOYTHHCkQYDnNw http://counselo.za.com/3A9SSOSGL9NHLbOBRwogEWRLCkto7C0J4tR3USxjzn17RiAWjQ 50% solids (45% mineral and 5% organic matter), and 50% voids (or pores) of which half is occupied by water and half by gas. The percent soil mineral and organic content can be treated as a constant (in the short term), while the percent soil water and gas content is considered highly variable whereby a rise in one is simultaneously balanced by a reduction in the other. The pore space allows for the infiltration and movement of air and water, both of which are critical for life existing in soil. Compaction, a common problem with soils, reduces this space, preventing air and water from reaching plant roots and soil organisms. Given sufficient time, an undifferentiated soil will evolve a soil profile which consists of two or more layers, referred to as soil horizons. These differ in one or more properties such as in their texture, structure, density, porosity, consistency, temperature, color, and reactivity. The horizons differ greatly in thickness and generally lack sharp boundaries; their development is dependent on the type of parent material, the processes that modify those parent materials, and the soil-forming factors that influence those processes. The biological influences on soil properties are strongest near the surface, though the geochemical in ------------------------------ Date: Wed, 22 Jun 2022 09:45:54 -0400 From: "Dangerous Hormones" Subject: Triggered by these 3 common fruits? Triggered by these 3 common fruits? http://counselo.za.com/ciyHYBXKDeBy3HG4PtynX_yxvK1xuWS57U9V2HZScGdXPCc http://counselo.za.com/qzv6gN9Oyc6ZAY0hzmV_KWYBepfA8Ydz3gB3dxVk5zLjigM re strongest near the surface, though the geochemical influences on soil properties increase with depth. Mature soil profiles typically include three basic master horizons: A, B, and C. The solum normally includes the A and B horizons. The living component of the soil is 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 de ------------------------------ Date: Wed, 22 Jun 2022 09:18:03 -0400 From: "live longer" Subject: 5,000 times stronger than worthless vitamin combo 5,000 times stronger than worthless vitamin combo http://naturallywork.za.com/7edlfWpbYpOtskEZ3F5RdmfyOeju45odPaYGzbihT9EO7r0tUQ http://naturallywork.za.com/Ziy2p_WKZlGRWVfVaZCIkP4n-ElQICqNtRgk1CxHBnkbPcV2WA osphere of soil, or soil gas, is very different from the atmosphere above. The consumption of oxygen by microbes and plant roots, and their release of carbon dioxide, decreases oxygen and increases carbon dioxide concentration. Atmospheric CO2 concentration is 0.04%, but in the soil pore space it may range from 10 to 100 times that level, thus potentially contributing to the inhibition of root respiration. Calcareous soils regulate CO2 concentration by carbonate buffering, contrary to acid soils in which all CO2 respired accumulates 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 ------------------------------ Date: Thu, 23 Jun 2022 03:14:31 +0000 From: Alyssa Denney Subject: **REPLY** We have an investment proposal for you that enables you to make a profit daily. Kindly contact for more details. ------------------------------ Date: Wed, 22 Jun 2022 08:37:10 -0400 From: "Every Disaster Claims" Subject: Your Family Is In Serious Danger (leaked report) Your Family Is In Serious Danger (leaked report) http://consulto.za.com/z4cv8B7mv5L4kh6sukHvR5JWdBpttqgx2ozs664SvaDbOcomUw http://consulto.za.com/T8pVR48fX4JSehzyELrbk17vpMdol4Y4Ow8zwYgwA2YQTgRb7g oil water content can be measured as volume or weight. Soil moisture levels, in order of decreasing water content, are saturation, field capacity, wilting point, air dry, and oven dry. Field capacity describes a drained wet soil at the point water content reaches equilibrium with gravity. Irrigating soil above field capacity risks percolation losses. Wilting point describes the dry limit for growing plants. Available water capacity is the amount of water held in a soil profile available to plants. As water content drops, plants have to work against increasing forces of adherence and sorptivity to withdraw water. Irrigation scheduling avoids moisture stress by replenishing depleted water before stress is induced. Capillary action is responsible for moving groundwater from wet regions of the soil to dry areas. Subirrigation designs (e.g., wicking beds, sub-irrigated planters) rely on capillarity to supply water to plant roots. Capillary action can result in an evaporative concentration of salts, causing land degradation through salination. Soil moisture measurementbmeasuring the water content of the soil, as can be expressed in terms of volume or weightbcan be based on in situ probes (e.g., capacitance probes, neutron probes), or remote sensin ------------------------------ Date: Wed, 22 Jun 2022 23:59:02 -0500 From: Ray Ban Subject: Ray-Ban Sunglasses Up To 90% Off!Top Quality Low Cost! Shop Online Now! Ray-Ban Sunglasses Up To 90% Off! Top Quality Low Cost! Shop Online Now! www.90off-rb.com ------------------------------ End of alt.music.moxy-fruvous digest V14 #9171 **********************************************