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"Wee Beasties" and other "Critters" in TP


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re: soil mites and gnats

 

I've found neem is a great for controlling fungus gnats. Soil drench with it or foliar spray and add the foliage eventually to be composted seems to help balance bugs in the compost heap too.

 

I have a lot of soil mites, compost really helps get them started in your TP pots. In the one pot where I added some bones and terra cotta I smashed up as well as charcoal, there's lots more soil mites than in the pot next to it. If this is good or bad remains to be seen. No spider mites so far, and the odd predator mite which is all good.

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I have found Neem a very effective deterrent to grasshoppers and many other pests.

My problem is when buying the oil how to dilute it.

 

As it is not an "official" pesticide/deterrent no instructions can be given.

 

 

Some info on soil as a"killer". !

Health: French Volcanic Clay Kills Antibiotic-Resistant MRSA Superbug

(NaturalNews) Researchers have discovered that a clay made from volcanic ash in France has powerful antibiotic properties and is capable of killing even antibiotic-resistant superbugs such as methicillin-resistant Staphylococcus aureus (MRSA). "It's...

French Volcanic Clay Kills Antibiotic-Resistant MRSA Superbug

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  • 2 weeks later...

Interesting local website of an international organisation

“Soil organisms create a living, dynamic system that needs to be understood and managed properly for best plant growth.

Understanding soil health requires knowing what organisms occur, which ones are working, how many are present and whether they are the right kinds for the desired plants.”

Soil Foodweb Institute Australia ::: Soil Foodweb Australia

Good Products for Soil Health

Our Good Products sections show the results of SFI assays of the microorganisms in a range of composts, compost teas and products that improve the soil foodweb. You can compare the results and find the manufacturers in your area most suited to your needs. Those listed have been approved by SFI as passing our rigorous standards and are involved in our ongoing Quality Assurance Programes.

Soil Foodweb Institute Australia ::: Soil Foodweb Australia

 

This is adownloadable book from Amazon.com

 

 

Digital Delivery

(How does this work?)

 

 

 

 

or Compare with similar items

Bacterial diversity of terra preta and pristine forest soil from the Western Amazon [An article from: Soil Biology and Biochemistry]

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Bacterial diversity of terra preta and pristine forest soil from the Western Amazon [An article from: Soil Biology and Biochemistry]

 (Digital)[/color][/b]

by J.-S. Kim (Author), G. Sparovek (Author), R.M. Longo (Author), W.J. De Melo (Author)

No customer reviews yet. Be the first.

List Price: $4.95

Price: $4.95

Availability: Available for download now. Ships from and sold by Amazon.com.

 

Edition: e-document (Learn more)

Book Description

This digital document is a journal article from Soil Biology and Biochemistry, published by Elsevier in 2007.

The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase.

You can view it with any web browser.

 

Description:

The survey presented here describes the bacterial diversity and community structures of a pristine forest soil and an anthropogenic terra preta from the Western Amazon forest using molecular methods to identify the predominant phylogenetic groups.

Bacterial community similarities and species diversity in the two soils were compared using oligonucleotide fingerprint grouping of 16S rRNA gene sequences for 1500 clones (OFRG) and by DNA sequencing.

The results showed that both soils had similar bacterial community compositions over a range of phylogenetic distances, among which Acidobacteria were predominant, but that terra preta supported approximately 25% greater species richness.

The survey provides the first detailed analysis of the composition and structure of bacterial communities from terra preta anthrosols using noncultured-based molecular methods.

http://www.amazon.com/Bacterial-diversity-pristine-forest-Western/dp/B000PC0KDU/ref=pd_bbs_sr_2?ie=UTF8&s=books&qid=1209654891&sr=8-2

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Interesting local website of an international organisation

 

Soil Foodweb Institute Australia ::: Soil Foodweb Australia

 

Soil Foodweb Institute Australia ::: Soil Foodweb Australia

 

This is adownloadable book from Amazon.com

 

 

Digital Delivery

(How does this work?)

 

 

 

 

or Compare with similar items

Bacterial diversity of terra preta and pristine forest soil from the Western Amazon [An article from: Soil Biology and Biochemistry]

See larger image

 

Bacterial diversity of terra preta and pristine forest soil from the Western Amazon [An article from: Soil Biology and Biochemistry]

 (Digital)[/color][/b]

by J.-S. Kim (Author), G. Sparovek (Author), R.M. Longo (Author), W.J. De Melo (Author)

No customer reviews yet. Be the first.

List Price: $4.95

Price: $4.95

Availability: Available for download now. Ships from and sold by Amazon.com.

 

Edition: e-document (Learn more)

Book Description

This digital document is a journal article from Soil Biology and Biochemistry, published by Elsevier in 2007.

The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase.

You can view it with any web browser.

 

Description:

The survey presented here describes the bacterial diversity and community structures of a pristine forest soil and an anthropogenic terra preta from the Western Amazon forest using molecular methods to identify the predominant phylogenetic groups.

Bacterial community similarities and species diversity in the two soils were compared using oligonucleotide fingerprint grouping of 16S rRNA gene sequences for 1500 clones (OFRG) and by DNA sequencing.

The results showed that both soils had similar bacterial community compositions over a range of phylogenetic distances, among which Acidobacteria were predominant, but that terra preta supported approximately 25% greater species richness.

The survey provides the first detailed analysis of the composition and structure of bacterial communities from terra preta anthrosols using noncultured-based molecular methods.

http://www.amazon.com/Bacterial-diversity-pristine-forest-Western/dp/B000PC0KDU/ref=pd_bbs_sr_2?ie=UTF8&s=books&qid=1209654891&sr=8-2

 

Great stuff MA! Thanks for sharing! ;)

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I was thumbing though an 'old' USA book on tissue culture and was suprised to find these ingredients listed as plant growth substances

  • Bacto (? brand name?) malt extract (Concentration 50-5,000mg/l)
  • Bacto Yeast extract (Concentration 50-5,000mg/l)
  • Caesin hydrolysate (Concentration 50-5,000mg/l)
  • Coconut milk/water (Concentration 100-150mg/l)
  • Orange juice (Concentration 50-300mg/l)

Can anyone shed any light on this?

 

Also iI speculated before about agar as a growing medium for wee beasties' as it is used in lab petrie dishes for growing "wee beasties" but now also tissue culture!

This book also suggests

  • "Gelrite" derived from bacteria (Pseudomonas sp.)
  • and various trade names of red algae (noble algae Simar Agar TC agar, etc

 

Does this stimulate any creative/speculative neurons in anyone's cranium?

Mine are just puzzled, but think there should be something in this information. (?)

 

BTW

If you want to import a plant into Australia Tissue Culture is the way to go. Customs and Agriculture far less feral as Tissue Culture is sterile.

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Bacto (? brand name?) malt extract (Concentration 50-5,000mg/l)

Bacto Yeast extract (Concentration 50-5,000mg/l)

Caesin hydrolysate (Concentration 50-5,000mg/l)

Coconut milk/water (Concentration 100-150mg/l)

Orange juice (Concentration 50-300mg/l)

 

You listed food for wee beasties. The list of what they'll recycle in soil and other substances is enormous.

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You listed food for wee beasties. The list of what they'll recycle in soil and other substances is enormous.

Yes I know.

There must be a zillion amino acids that they eat

I was just surprised to see the above listed in a Tissue Culture Book ??!!

Orange Juice?

Coconut milk???

Do they have a full 'English Breakfsst' (Caesin sausages???)

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Yes I know.

There must be a zillion amino acids that they eat

I was just surprised to see the above listed in a Tissue Culture Book ??!!

Orange Juice?

Coconut milk???

Do they have a full 'English Breakfsst' (Caesin sausages???)

:) Breakfast with the beasties.... Good one, M,ca!

 

I think this is a link to that Springer article, above.

http://www.ambientenet.eng.br/TEXTOS/SOILBIOLOGY20073.PDF

...there's another half hour of my life I won't get back. :smart:

 

The relationship between organic matter inputs from different overstory trees, rhizosphere effects, and the bacterial community composition of forest soils is still not understood, but likely contributes to differences in diversity and community composition along the forest floor.
Rhizosphere! What a neat word! That'll be running thru my head all day....

 

Thanks for pointing out that "download from Amazon" stuff.

I'm trying to figure that out.... :alien_dance:

~Later....

:lol:

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Rhizosphere = round Rhizos?

 

Eric's "wee beastie" Condos with in built security systems against 'bad guys'

Mechanism 2: Biochar alters the activity of other

micro-organisms that have effects on mycorrhizae

. . .

Hyphae and bacteria that colonize biochar particles (or other porous materials) may be protected from soil predators (Saito 1990; Pietikäinen et al. 2000; Ezawa et al. 2002), which includes mites, collembola and larger (>16 μm in diameter) protozoans and nematodes.

The documented physical parameters of the biochar particles themselves make this mechanism plausible.

The average sizes of soil bacteria and fungal hyphae range from 1 to 4 μm and 2 to 64 μm, respectively, with many fungal hypha being smaller than 16 μm in diameter (Swift et al. 1979).

Additionally, the average body-size of a soil protist is between 8 to 100 μm, while the average body size of soil micro-arthropods ranges from 100 μm to 2 mm (Swift et al. 1979).

In contrast, the pore diameters in a biochar particle can often be smaller than 16 μm in diameter (Kawamotoet al. 2005; Glaser 2007; Hockaday et al. 2007).

Based on the differences in the body sizes across these different organisms, it is clearly possible that many of the pores within a biochar particle are large enough to accommodate soil microorganisms, including most bacteria and many fungi, to the exclusion of their larger predators.

Thus, the biochar would be acting as a refuge for MHB, PSB and mycorrhizal fungi.

 

Supporting evidence for this hypothesis comes from Saito (1990), Gaur and Adholeya (2000) andEzawa et al. (2002) who all showed that AMF readily colonize porous materials and were capable of heavily colonizing biochar particles in the soil.

 

Lastly, Pietikäinen et al. (2000) and Samonin and Elikova (2004) showed that bacteria readily colonized biochar particles; these may include MHB and/or PSB.

http://www.css.cornell.edu/faculty/lehmann/publ/PlantSoil%20300,%209-20,%202007,%20Warnock.pdf

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Just found this interesting Australian site.

Well worth exploring.

 

LeftClick: Composting with worms-- another sustainability lesson from Cuba

Wednesday, May 7

Composting with worms-- another sustainability lesson from Cuba

 

The English Green Party's Derek Wall dug up (so apt!) this piece by Matthew Werner on worm farming in Cuba for compost week.Worms as Charles Darwin insisted are important critters.

 

"Food for worms..." can be almost anything as the medieval Church and Shakespeare's Hamlet have pointed out. Food like...very dead human beings.

 

 

Not where he eats, but where he is eaten:

a certain convocation of politic worms are e'en at him. Your

worm is your only emperor for diet: we fat all

creatures else to fat us, and we fat ourselves for

maggots: your fat king and your lean beggar is but

variable service, two dishes, but to one table:

that's the end.

 

Worms are also highly efficient carbon sequestors. By taking organic matter underground, the worms reduce carbon release into the atmosphere as carbon dioxide and worm farming is akin, in my estimation, to such practices as Agri Char (aka Terra Preta) in the role it could play -- rather quickly -- to ameliorate global warming.But no major Vermicompost project has been initiated with that thesis in mind.

 

David Murphy's book , Organic Growing With Worms addresses that possibility in its pages with great verve such that the irrepressible Peter Cundall writes in regard to it:

 

"This is an amazing, inspiring book..it should be on the bookshelf of every farmer, gardener, conservationist, scientist or anyone who comprehends the environmental dangers now threatening all life forms on earth."

 

Murphy writes that "...if [the world's agricultural soil] were raised to 5 per cent [organic matter] to a depth of 25 cm, 150 billion tonnes of carbon dioxide would be sequestered into the soil ".

 

Healthy soil could sequester up to 350 tonnes of carbon per hectare (Jones 2007), this being equivalent to about 1,285 tonne of carbon dioxide per hectare removed from atmosphere....This exceeds the estimated 15 billion tonnes per annum global emissions of carbon dioxide from all sources (Murphy 2005) 10 times over.

 

Hence soil represents the largest potential sink (storage capacity) for carbon - if natural soil quality is restored and maintained -- Sunnyside Projects.

 

*Yep. Worms are really something to get excited about -- not only as a means to bed down waste (3% of national carbon emissions) but also as a means to invigorate the extremely poor nature of Australian soils while helping to reduce the share agriculture plays in our total carbon emissions. -- 16% from Agriculture (larger than transport-- 13%-- and second only to stationary energy ).

 

 

Trends in carbon dioxide equivalent emissions from the agricultural sector, 1990-2004

 

 

Sixty percent of emissions from the agricultural sector come from enteric fermentation in livestock. These are emissions associated with microbial fermentation during digestion of feed by ruminant (mostly cattle and sheep) and some non-ruminant domestic livestock. Emissions associated with agricultural soils (e.g. disturbance of land by cropping, improved pastures and the application of fertilisers and animal wastes) and prescribed burning of savannas also account for a significant proportion of net emissions.

 

While enteric fermentation is the main driver of emissions from agriculture, to replace that caloric output with plant foods behooves a major shift in soil management .

 

--Dave Riley

--

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  • 3 weeks later...
The activity of soil organisms can be divided into four functions:

1. Regulation of OM turnover & nutrient cycling,

2. Biological degradation

3. Maintenance of soil structure, and

4. Interaction with plants.

1a. Organic Matter (OM) Turnover:

• Carbon is a core element of OM and a vital energy source for soil biota.

• By decomposing OM the soil biota gain access to this carbon.

• Microbial biomass, the population of micro-organisms, acts as the engine for

OM turnover and nutrient release.

• Soils with high levels of OM support a greater number and a more diverse

range of biota.

• Where OM energy is plentiful, crop residue decomposition and OM

accumulation will occur.

• Specific organisms breakdown different types of OM. e.g. cellulolytic micro-

organisms only decompose cellulose and not lignin.

• The rate of OM breakdown relates to the soil environment, the number and

type of organisms present and the chemical structure of the plant residues.

Breakdown may occur in months or several thousand years.

1b. Transformation of Nutrients:

• The conversion of OM, by soil organisms, to available nutrients is called

mineralisation. This process is a key element of soil fertility.

• Whilst decomposing OM to obtain carbon, other nutrients are released.

These may be: soluble and leached (e.g. nitrate [NO3]), volatile and lost to

the atmosphere (e.g. nitrogen as N2 & N2O, sulphur as H2S) or readily

available to the plant (e.g. nitrates, phosphates and sulphates).

• In order to increase the up-take of a specific nutrient, many plants form

mutual relationships (symbioses) with soil micro-organisms. Examples of

symbiotic relationships include: legumes with the bacteria Rhizobium

species to fix atmospheric nitrogen gas, and most crops with mycorrhizal

fungi to absorb phosphorus and other nutrients from the soil environment.

• Mycorrhiza have been found to improve plant uptake of phosphorus. This is

thought to be due to the vast ‘collection structure’ provided by the hyphal

network of fungi.

. . .

 

[url=http://72.14.253.104/search?q=cache:AYNOHBwvwTYJ:www.csiro.au/files/files/pcz9.pdf+CSIRO+no+till+farming+soil+microorganisms&hl=en&ct=clnk&cd=4&gl=au&client=firefox-a]The

 

The relationship between agricultureand soil organisms

Tillage:

Cultivation alters the physical, chemical and biological components of the soil

system. No-till, direct-drill systems result in significant differences in soil

organism activity compared to conventional deeper tillage.

No tillage:

• OM levels are high and micro-organisms become concentrated at the soil

surface.

• Residue decomposition and nutrient mineralisation is slower.

• Fungal hyphae are more prolific in the top 5cm of soil. This is beneficial in

terms of desirable fungi such as mycorrhizae but negative in relation to

pathogenic fungi such as Rhizoctonia.

• Fungal feeding nematodes, protozoa and macro fauna increase.

• 10 - 100 times more fungal feeding protozoa were counted under no-till and

stubble retention treatments. These may provide controls for pathogenic

fungi.

• Narrow points on cultivators used at seeding result in soil disturbance below

the seed. This in combination with a three week chemical fallow, prior to

seeding, reduces the severity of the pathogenic fungus Rhizoctonia .

• Deep burrowing earthworms in direct drilled plots improve soil structure

assisting root growth and increasing the yield of annual crops.

 

Conventional Tillage:

• This favours organisms with short generation times, rapid dispersal and high

metabolic rates. Bacteria and bactivorous fauna are dominant in cultivated

soils.

• Fungal hyphae are broken by cultivation and therefore reduced.

• Organisms are distributed more deeply into the ploughed layer .

• Residue decomposition and nutrient mineralisation is more rapid due to

better soil-stubble contact.

• The rapid activity results in a higher level of breakdown and a lower level of

OM accumulation.

• Earthworm populations significantly decrease.

• Increased cultivation has been shown to reduce the number of root lesion

nematodes, but no effect on cereal yield has been recorded.

influence soil biota activity?

Stubble incorporation favours bacteria and bactivorous fauna whereas stubble left on soil surface supports more fungi and fungivorous fauna.

. . .

http://72.14.253.104/search?q=cache:AYNOHBwvwTYJ:www.csiro.au/files/files/pcz9.pdf+CSIRO+no+till+farming+soil+microorganisms&hl=en&ct=clnk&cd=4&gl=au&client=firefox-a

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  • 3 weeks later...

:eek:Wee Beasties to pyrolysis to charcoal to soil to more Wee Beasties?

;)

When people think of capturing sunlight energy in biomass, they focus on plants, which are familiar. However, plants are quite inefficient at capturing sunlight energy and turning it into biomass that can be used a fuel,"

. . .

"Photosynthetic bacteria can capture sunlight energy at rates 100 times or more greater than plants, and they do not compete for arable land," Rittmann said.

This high rate of energy capture means that renewable biofuels can be generated in quantities that rival our current use of fossil fuels.

 

In addition, non-photosynthetic microorganisms are capable of converting the energy value of all kinds of biomass, including wastes, into readily useful energy forms, such as methane, hydrogen, and electricity.

 

"Microorganisms can provide just the services our society needs to move from fossil fuels to renewable biofuels," said Rittmann.

"Only the microorganisms can pass all the tests, and we should take full advantage of the opportunities that microorganisms present."

 

Journal reference:

 

1. Rittmann et al. Opportunities for renewable bioenergy using microorganisms. Biotechnology and Bioengineering, 2008; 100 (2): 203 DOI: 10.1002/bit.21875

 

Adapted from materials provided by Arizona State University, via EurekAlert!, a service of AAAS.

Harnessing Microbes To Meet Our Future Energy Needs

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  • 2 weeks later...

I watched a show last night on ABC TV on the Rice Research Institute in the Philippines. A lot of Oz researchers are working there.

 

One researcher gave a long list of all the factors affecting rice production, genetics, pests, disease resistance etc., etc., at least 20 or more factors/variables.

 

Yet she did not mention "soil" once.

 

No mention of Rice Hull Charcoal now being exported.

 

How sad.

:shade: : (: :hihi::( : (: :hihi::( : (: :(:( : (: :(:( : (: :(:( : (: :( :( : (: :(

 

Here is a website that will keep you studying for a decade.

Krasil'nikov: TOC

SOIL MICROORGANISMS AND HIGHER PLANTS
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  • 4 weeks later...
]

What are the functions that the microbes perform that cannot be accomplished by synthetic or mineral products?[/b]

The following are the functions that only the biological life in the soil can perform:

 

1. Decomposition of crop residues, manure and other organic matter to humus by the microbes for use by the plants.

2. Retention of nutrients in humus and in the microbes themselves that recycles.

3. Nutrient recycling by the biological food chain as microbes consume each other and nutrients are released to the plants.

4. Biological control of plant and soil diseases through biological pathogen suppression.

5. Production of plant growth regulators by the microbes that affect plant production.

6. Soil structure and tilth development produced by biological byproducts of the microbes.

7. Biological clean up of herbicide of pesticide carryover through degradation by the microbes into harmless byproducts.

 

What is the process the plant uses to support the microbial population?

In the photosynthesis of plants, photosynthates (complex sugars) are produced in the leaves. The plants send as much as 50% of these complex sugars down, passing out of the root into the soil to feed the microbes. With this energy received from the plant, the microbes convert essential nutrients from synthetic fertilizers along with nutrients and mineral reserves held in humus and other carbon-based compounds.

 

This biological partnership between plants and microbes is mutually beneficial. The plants feed the microbes the energy they need and the microbes feed the plants the variety of nutrients the plants need.

p

 

Why can't plants obtain all of the nutrients they need from synthetic fertilizers?

Plants feed at the second table. The plant feeds on what the microbes provide. Plants are poor foragers and scavengers of nutrients in fertilizers compared to microbes. Microbes have the capacity of "mining" or releasing nutrients from soil particles that are unavailable or "tied-up". Since microbes need carbon, nitrogen, phosphate, potassium and minor nutrients and trace minerals, they digest these nutrients and change them to a chelated or carbon-based form for the plants.

The microbes rely on plants to provide the complex sugars released from plant roots to support the microbes ability to provide nutrition for the plants.

 

Plants rely on the microbes to digest organic matter into humus that contains the nutrients in stable humic compounds.

The plant uses these stored and stable nutrients through the symbiotic relationship with the microbes.

The carbon and the balanced carbon/nitrogen relationship of microbes are vital in maintaining healthy, productive soil.

How do microbes function as the digestive system for plants?

The rhizosphere (microbes on or near the roots) is the digestive system for the plants. This zone of soil next to plant roots supports a much higher population of microbes than the soil even a short distance away from the roots. The numbers of microbes on or near the roots is up to 100 times greater than just 1/4" away from the root.

This high population of microbes near plant roots is varied in composition and activity.

This is the area of greatest digestion of minerals and nutrients by microbes that is made available to the growing plants.

These microbes live in a symbiotic relationship with the plant roots, using as a source of energy the varied organic nutrients that the roots discharge to feed the microbes.

These complex sugars stimulate a variety of microbes to obtain nutrients the plant needs for balanced nutrition.

Microbes have the chelating capacity for converting inorganic minerals to chelated or organic-based minerals plants can use to improve balanced nutrition.

BioFlora - Nature Knows Best

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