Jacky said:I would like to suggest that we start a parallel discussion on how Bob Morriss would use charred materials in his large scale "Bio Organic Fertilizer" (BOF) process for composting.
This is a good idea, Maybe what has been presented could be of value to Bob, if it can be applied to his process.I want to second your suggestion that others consider large scale production using pyrolysis. That is what we will be doing weith our system, both to provide large quantities of charred material and to produce bio-deisel form the exhaust.
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To that end, I was thinking about already-collected materials in this
country (the U.S.), e.g., what you can find in forestry dumps.
I am curious as to whether anyone has experience with smoldering
forestry waste, especially fallen leaves, or smaller radial twigs?
Would one get a suitable charcoal product? How would you construct the
pile to get it lit, but still have it smolder in the absence of oxygen.
Would leaf charcoal have the characteristics you want? Why does
compost leaves give you humus, but no charcoal? Would pyrolysis of
leave give you a suitable product?
Also, I'm reading 1491, which I'm sure many of you have. The author
goes into detail about the Amazonian terra preta soils. It would be
nice if one of us would contact some of the researchers at Cornell or
elsewhere to see if they would join the discussion. I'm willing to do
that if no one else has contacts or relationships. I am also willing
to leave the academics out of this discussion if other feel that way.
Cheers,
Dan Nagengast
On Aug 19, 2007, at 12:18 AM, Jacky Foo wrote:
>
>
> On 19/08/07, Bob Morriss <rbmor...@att.net> wrote:
> >I believe we need to find a way to incorporate them into
> >a large scale system.
>
> Dan N provided us with the idea that charred materials from
> pyrolysis could be a source.
>
> This would mean integrating bioenergy production (using pyrolysis)
> with solid waste recycling via composting at a large scale. The
> machinery to do all these is available and all these processes are
> already happening
> separately. It is just to bring all these together.
>
> Since we are very much done with Mel's method of producing dark earth
> soil (small scale) and as he does not have any yields data for
> discussion, I would like to suggest
> that we start a parallel discussion on how Bob Morriss would use charre
> d materials in his large scale "Bio Organic Fertilizer" (BOF)
> process for composting.
>
> regards
> jacky
>
> >
>
Dan Nagengast
785-748-0959
785-748-0609 fax
nage...@earthlink.net
www.kansasruralcenter.org
Hello all,
To that end, I was thinking about already-collected materials in this
country (the U.S.), e.g., what you can find in forestry dumps.
I am curious as to whether anyone has experience with smoldering
forestry waste, especially fallen leaves, or smaller radial twigs?
Smoldering happens in the air. If you are talking about using a system such as is used for primitive production of charcoal, it would be too much work for what you would get. Materials such as twigs, leaves and other small biomass, need to be charred in closed system with the material compresed as much as possible.This allows collection of the exhaust gasses for other uses, such as wood vinegar (a fermented liquid smoke that is a good fertilizer and pesticide) or bio-deisel.
Would one get a suitable charcoal product? How would you construct the
pile to get it lit, but still have it smolder in the absence of oxygen?You get a usable charcoal from pyrolysis. The Kayapo burn various leaves and use the ash. That does not produce charred material however.
Would leaf charcoal have the characteristics you want?
Charred leaves should be beneficial to the production of dark earth soils. It is probably not persistant for thousands of years, but may be for hundreds of years. Research is needed in this and other areas.
Why does compost leaves give you humus, but no charcoal?
Aerobic composting, the fast type done in the presence of air, yields little humus. Most humus is produced during the slow decomposition done by abaerobes. Charcoal is produced when the material is heated with insuficient Oxygen to burn the Carbon. So, it needs to be produced seperately by pyrolysis.I have imbedded the Humus document into this letter below. It might be useful for you to review it.melHumus in Tropical and Subtropical SoilsHumus in Wet Tropical EnvironmentsWet land tropical forests appear to be growing on highly fertile soils. Thetruth is that there is a thin layer of quickly decomposing organic matteron the surface of otherwise low fertility soil. The warm, moist, highlyoxygenated environment on the forest floor of tropical forests, providesoptimum conditions for the fungi and bacteria which decompose thelayer of mulch that accumulates at the base of the trees.Also present in this decomposing layer of organic matter are beneficialorganisms that quickly make the newly released nutrients available to thetree roots. Nutrient cycling in such an environment takes place quickly.The formation and deposition of humus is almost non-existent. This iswhy newly cleared tropical forest cannot sustain production for morethan a few years. There is no humus to maintain fertility.The Composition of HumusHumus is an ill defined substance. It is known to be an essential componentof healthy soils. It improves the structure of soils, provides appropriatehabitats for beneficial micro-organisms and effectively stores energy andnutrients for later use. It clumps sand particles and separates clay particles.But, humus is so complex and varied, from one environment to another andfrom one mix of plants to another, that it is impossible to establish an exact description of its composition. Even within the same plant community, the difference in maturity of the plants can alter the composition of humus.Humus is composed of organic matter derived from plants and animalsthrough the decomposing actions of microbes. It's molecules come in manyforms and it is dark in color. It is also stable in comparison to other organic materials such as manure or compost, which are more prone to decomposition.Although considered stable over long periods of time, humus is neveractually an end product. It continually changes its complex structure overtime. This applies more to newly formed humus than to that which hasexisted for decades or centuries, however. That humus is quite stable.In general, the longer it persists, the more stable it becomes. But, whendisturbed by tillage, broken by other mechanical action, exposed to solarradiation or heat from fire or the sun, even old humus can be altered somuch that it can be utilized by the organisms responsible for decomposition.Formation of HumusAny given biomass is composed of various carbohydrate molecules. Some,such as sugar, starch and some proteins, provide easily digested energysources for bacteria. Fungi can use these same substances as well ascellulose and hemi cellulose for the same purpose.Other organic compounds are not so easily decomposed. Fats, lignins andwaxes are much more resistant to decay. A large percentage of thecarbohydrate molecules in humus are made up of these components, not intheir original form, but altered by the decomposition process. Others are substances produced by the organisms themselves during decomposition.Bacteria, in general, produce sticky substances that cause carbohydratemolecules to clump together. But, it is mainly during the slowdecomposition, brought about by anaerobes, that these glue likesubstances form the stable bonds that produce large quantities of humus.The Effects of Farming Methods on HumusProductive soils should have at least 5% organic matter content. Thisshould be composed of thousands of different bacteria and fungalspecies, plant and animal tissues in various states of decomposition andstable humus. Undisturbed soils, with plenty of decomposing organicmatter on the surface, normally provide a good environment for themaintenance of soil organic matter, but not necessarily of humus.Conventionally farmed soils are low in all three of these categories oforganic matter. Breaking apart the soil damages fungal mycelia,earthworms and humus. Exposure to high concentrations of Oxygenincreases the rate of decomposition. Exposure to the heat and radiationof the sun kills micro-organisms and further damages the structure ofhumus, making it susceptible to decomposition by soil organisms.Tillage also exposes the soil to erosion from rain and wind. This furtherdecreases the quantity of organisms, decomposing tissues and humus, asit is washed or blown away. With soil erosion, the productive capacity ofthe land is lost along with the potential wealth of those farming the land.The use of concentrated fertilizers can further damage the organic mattercontent of soils by speeding up decomposition, through the introduction oflarge quantities of Nitrogen into the soil. These fertilizers also acidify thesoil and can kill necessary micro-organisms. The use of pesticides,herbicides and fungicides can also kill large numbers of soil organisms.Humus in Tropical SoilsThe warm temperatures and moist conditions of disturbed tropical and subtropical soils are not conducive to the production, accumulation orpersistence of humus in soils, especially in highly oxygenated sandy soils.Under warm, humid, high Oxygen conditions, aerobic organisms quickly decompose organic matter. The bacteria and fungi which thrive in thesehighly oxygenated, warm, humid conditions produce little humus. Fastcomposting thoroughly decomposes the biomass and releases the mineral components, which are used as food by the decomposers.Even without tilling the soil, humus does not accumulate in many tropicaland sub-tropical environments. At a certain combination of temperature,Nitrogen level, Oxygen level and humidity, humus is not produced. So, it is especially unusual to find high levels of humus that has been stable for over500 years in the midst of the Amazon Basin. The farmers who producedthese soils achieved something modern science has not been able to duplicate.In order to produce substantial amounts of humus in tropical soils, theremust be some control over the temperature and Oxygen level in the soil.This was apparently accomplished by these ancient farmers. They builtsoils rich in both charcoal and humus. Both are important for conditioningthe soil, for storing nutrients and for supporting micro-organisms.Producing Humus under Warm, Humid ConditionsShading of the soil with a thick organic mulch or cover crop cansignificantly lower the temperature. Burying organic matter well belowthe surface of the soil can limit oxygen. Many bacteria that are classifiedas anaerobes can also function in the presence of decreased amounts ofOxygen, to produce humus.It is hard to maintain organic matter content in any cropped soil. Perennial farming systems that require a high concentration of trees, such as shadegrown coffee or Cacao production, provide the proper model for maintaining adequate levels of soil organic matter in tropical soils. The key toaccomplishing this in other cropping systems is to alter their management to provide a similar environment at and, preferably, below the surface of the soil.The use of mulched raised beds, built on the level, can prevent erosion andprovide a cool, moist, shaded environment with plenty of food for soilorganisms. This farming system can significantly increase the amount oforganic matter contained in organisms and decomposing plant and animaltissues. But, the highly oxygenated environment restricts the production ofstable humus in the soil.Producing Dark Earth SoilsThousands of years ago the Native American Farmers of the Lower AmazonRiver Basin discovered a way of improving the structure of their soils and maintaining fertility, despite the high levels of precipitation in the region.They accomplished this through the incorporation of charred organic matterand through the production of large amounts of humus. They did this in an environment where humus is normally almost non-existent. We need to re-discover their technology.Burying organic matter below a layer of soil, thus reducing theavailability of Oxygen, should significantly increase the amount of humusproduced by aerobic organisms. Of course, the amount of Oxygenreaching this layer depends on the nature of the soil itself; varying as aresult of the percentages of clay and sand.A layer of organic matter that includes adequate Nitrogen, Carbon andmoisture, for a slow decomposition by anaerobic organisms, shouldprovide an environment in which nutrients are released, but are held inplace by organisms and by the humus they produce.The addition of Charred biomass should significantly increase the ability ofthe soil to retain nutrients in the root zone. Not all charred materials are thesame, however. Those produced from lignins are more persistent than those madefrom hemi-cellulose, for instance. But, both should have the capacity forbehaving as Chelating agents. Finer particles should also provide moresurface for holding nutrients than would large chunks.Another potential benefit from such a system is the Carbon sequestration that results from burying charred biomass within the soil. Incorporating charcoal, produced from waste products or from quick growing tree species, could lock away appreciable amounts of atmospheric Carbon, if done on a large scale.
Thanks Mel.
Dan
On Aug 20, 2007, at 11:09 AM, Mel Landers wrote:
> Hi,
>
> I will comment in bold between the questions below
>
> Daniel Nagengast wrote:
Dan Nagengast
785-748-0959
785-748-0609fax
nage...@earthlink.net
www.kansasruralcenter.org