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As these organisms eat, grow, and move through the soil, they make it possible to have clean water, clean air, healthy plants, and moderated water flow.
The soil food web is the community of organisms living all or part of their lives in the soil. As organisms decompose complex materials, or consume other organisms, nutrients are converted from one form to another, and are made available to plants and to other soil organisms. Organic matter is many different kinds of compounds - some more useful to organisms than others.
Intensive tillage triggers spurts of activity among bacteria and other organisms that consume organic matter (convert it to CO2), depleting the active fraction first. Soil organic matter is the storehouse for the energy and nutrients used by plants and other organisms. Living organisms: Bacteria, fungi, nematodes, protozoa, earthworms, arthropods, and living roots. Active fraction organic matter: Organic compounds that can be used as food by microorganisms.
Particulate organic matter (POM) or Light fraction (LF) organic matter: POM and LF have precise size and weight definitions. Bacteria are abundant around this root tip (the rhizosphere) where they decompose the plentiful simple organic substances.
Many different organisms are active at different times, and interact with one another, with plants, and with the soil.
The living component of soil, the food web, is complex and has different compositions in different ecosystems.
Despite a global increase in meat consumption, humans are far from the top of the food chain. Sorry fellow humans but, contrary to the popular idiom, we aren’t at “the top of the food chain.” It turns out we’re actually somewhere in middle. While it’s good novel fun to strip homo sapiens of its illegitimate title of apex predator, the purpose of the study wasn’t just to provide scientists with another opportunity to correct laypeople in conversation. Among the low-but-increasing group 2 were China and India, which are driving that upward trend.
All this shifting meat consumption is a concern because, despite our middling trophic level, we’re quite good at sucking up resources.
As a child, Alex Reshanov was told by grown-ups that she should consider becoming a lawyer (tendency to argue) or a comedian (frequent joking), so naturally she opted for science writing. This is a side by side view of  two popular food grade Diatomaceous earth’s on the market. Food Grade Diatomaceous Earth by Grandpa’s is a 100% natural product, meaning it is in its purest form, nothing has been added to it, it has not been chemically or heat treated, just mined and ground up into a fine powder, and packaged for you. Pool grade Diatomaceous Earth is calcined (Meaning it has with gone some serious heat treating) this turn’s a lot of the natural Amorphous Silica into crystalline silica, which is very harmful to Humans and Pets, This stuff is no joke, use the right precautions when handling Pool Grade Diatomaceous Earth. Grandpas Food Grade Diatomaceous Earth must have less than 1% Crystalline Silica to be considered SAFE or Food Grade But Pool Grade can contain anywhere from 1% to 75% Crystalline Silica. My recommendation would be not to go breathing in all the Food Grade Diatomaceous Earth you can, but it really won’t harm your lungs anymore then breathing in other fine dust or powder, just be smart.
They range in size from the tiniest one-celled bacteria, algae, fungi, and protozoa, to the more complex nematodes and micro-arthropods, to the visible earthworms, insects, small vertebrates, and plants.
Soil organisms decompose organic compounds, including manure, plant residue, and pesticides, preventing them from entering water and becoming pollutants.
A food web diagram shows a series of conversions (represented by arrows) of energy and nutrients as one organism eats another.
Most other soil organisms get energy and carbon by consuming the organic compounds found in plants, other organisms, and waste by-products.



As individual plants and soil organisms work to survive, they depend on interactions with each other. In general, soil organic matter is made of roughly equal parts humus and active organic matter. Practices that build soil organic matter (reduced tillage and regular additions of organic material) will raise the proportion of active organic matter long before increases in total organic matter can be measured. Bacteria, fungi, and other soil dwellers transform and release nutrients from organic matter. The active fraction changes more quickly than total organic matter in response to management changes. They are thought to represent the active fraction of organic matter which is more difficult to define. Humus is not readily decomposed because it is either physically protected inside of aggregates or chemically too complex to be used by most organisms. Each species and group exists where they can find appropriate space, nutrients, and moisture.
Fungi are common decomposers of plant litter because litter has large amounts of complex, hard-to-decompose carbon. Biological activity, in particular that of aerobic bacteria and fungi, is greater near the surfaces of soil aggregates than within aggregates.
Those arthropods and nematodes that cannot burrow through soil move in the pores between soil aggregates.
In temperate systems, the greatest activity occurs in late spring when temperature and moisture conditions are optimal for growth. Even during periods of high activity, only a fraction of the organisms are busily eating, respiring, and altering their environment. The combined result is a number of beneficial functions including nutrient cycling, moderated water flow, and pest control.
Management of croplands, rangelands, forestlands, and gardens benefits from and affects the food web. So says a 49-year analysis of human food consumption across 176 of the world’s 196 countries.
Shouldn’t I at least be a 3?” To explain why the answer is no, let’s look at how trophic level is determined. Calculating the human trophic level (HTL) allows us to better understand our species’ impact on ecosystems and the planet’s resources.
Considering the energetic costs of dining at higher trophic levels, the better question about that 2.21 might now be, “why so high?” The main reason is volume. According to the study, humans use 25% of the net primary production (that finite amount of planty energy we discussed earlier), and food production accounts for 35-40% of that allocation. In 2010, she started a personal blog, Blogus scientificus, as an outlet for her diverse scientific interests, random pop culture trivia and various phobias.
Once done they googled about how Diatomaceous Earth works, only to find out the should not have used pool grade, (they dusted a hazardous substance all over their home) They then had to wear safety masks while at home day and night and while the rigorous process of cleaning it up. They sequester nitrogen and other nutrients that might otherwise enter groundwater, and they fix nitrogen from the atmosphere, making it available to plants. A few bacteria, called chemoautotrophs, get energy from nitrogen, sulfur, or iron compounds rather than carbon compounds or the sun. As soil organic matter levels rise, soil organisms play a role in its conversion to humus - a relatively stable form of carbon sequestered in soils for decades or even centuries.
Because POM or LF is larger and lighter than other types of soil organic matter, they can be separated from soil by size (using a sieve) or by weight (using a centrifuge). Humus is important in binding tiny soil aggregates, and improves water and nutrient holding capacity.


They occur wherever organic matter occurs - mostly in the top few inches of soil (see graph below), although microbes have been found as deep as 10 miles (16 km) in oil wells. It is teeming with bacteria that feed on sloughed-off plant cells and the proteins and sugars released by roots.
Within large aggregates, processes that do not require oxygen, such as denitrification, can occur. Organisms that are sensitive to desiccation, such as protozoa and many nematodes, live in water-filled pores. The next unit of the Soil Biology Primer, The Food Web & Soil Health, introduces the relationship of soil biology to agricultural productivity, biodiversity, carbon sequestration and to air and water quality. The study marks the first time anyone took the trouble to calculate human trophic level – a measurement of a species’ position in the food web.
All the plants in the world can only produce so much energy (aka food), and some of this energy is lost at each stage as it travels through the food web.
As a species, we aren’t really eating animals with higher trophic levels, we’re simply eating more meat (and animal products) overall.
Given that agriculture isn’t even our only drain on global resources, the fact that we’re not at the top of the food chain is probably a good thing. Many organisms enhance soil aggregation and porosity, thus increasing infiltration and reducing runoff. In turn, soil organisms support plant health as they decompose organic matter, cycle nutrients, enhance soil structure, and control the populations of soil organisms including crop pests.
Bacteria tend to use simpler organic compounds, such as root exudates or fresh plant residue. Bacteria cannot transport nitrogen over distances, giving fungi an advantage in litter decomposition, particularly when litter is not mixed into the soil profile. The remaining six units of the Soil Biology Primer describe the major groups of soil organisms: bacteria, fungi, protozoa, nematodes, arthropods, and earthworms.
Plants (and other “primary producers”) are a 1; they make their own food and, excluding the handful of carnivorous species, they don’t eat anyone else.
In terms of efficiency, more plants are required to provide a population with an all cow diet than with an all plant diet. Fungi tend to use more complex compounds, such as fibrous plant residues, wood and soil humus. Thus, much of the nutrient cycling and disease suppression needed by plants occurs immediately adjacent to roots. However, bacteria are abundant in the green litter of younger plants which is higher in nitrogen and simpler carbon compounds than the litter of older plants. That’s comparable to pigs and anchovies (the researchers’ examples), animals that are coincidentally also both popular pizza toppings (my commentary). For the rest of us, our level is calculated as 1 plus a weighted average of the trophic levels of whatever it is we eat.
Bacteria and fungi are able to access a larger surface area of plant residue after shredder organisms such as earthworms, leaf-eating insects, millipedes, and other arthropods break up the litter into smaller chunks. Species with the highest trophic levels are not just carnivores, they’re carnivores that eat other carnivores.
But if we were determined to climb the trophic ladder, we might want to dispense with cows altogether and focus on eating things like lions and bald eagles.




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