Here is the fourth entry in a series exploring new and orphaned knowledge of nitrogen cycling to update the view of the forest gardener – there are many articles to be written so stay tuned.
In this article, we’ll take a step back and look at the bigger picture of the local nitrogen cycle, and see broadly how the various inputs and outputs interact. This article will also be written a bit less in-depth than the previous ones, because we’re not covering new ground (where we require extraordinary evidence for extraordinary claims).
Why do we care about nitrogen at all? Nitrogen is one of the main limiting nutrients for plant growth in a wide variety of ecosystems around the world. It can be very soluble (when present as nitrate) and can easily leach too deeply to be captured by plant roots. It can’t be mined from the subsoil by deep-rooted plants (unlike phosphorus). Any major ecosystem disturbance (deforestation, excessive fertilization) can see lots of soil nitrogen escape via runoff, leaching or denitrification processes.
Luckily, there is a network of processes that brings nitrogen both into, and out of the ecosystem – this is called the nitrogen cycle. This cycle operates on many different scales. At the global scale, nitrogen is present in the atmosphere (in practically inexhaustible amounts – 79%), which is fixed by nitrogen-fixing bacteria into a solid-form, taken up by plants, and then as the plants die, the nitrogen is decomposed from organic compounds, and eventually denitrified and re-enters the atmosphere.
The nitrogen cycle also operates at a much smaller scale, cycling within an ecosystem whereby nitrogen travels from the plants, back to the soil, and then back to the plants – we can think of this as the local nitrogen cycle.
The Local Nitrogen Cycle
At the level of scale of a forest garden, the amount of available nitrogen is dominated by the rates of nitrogen transfer between plants and soil. This is really a special case of what’s called a nutrient cycle [Nutrient cycle].
To gain a deeper understanding of the local nitrogen cycle, we need to know what are the pieces that make it up, and what are the connections between these pieces. These can be thought of as ‘pools’ and ‘flows’ (flows can be further broken down into external inputs, external outputs and internal flows). A nitrogen pool is a place where nitrogen has gathered, and a flow is a channel that moves nitrogen from one pool to another. Click on the graphic below to read more about nitrogen pools and flows that are important within the scale of a forest garden.
Associative nitrogen fixation in soil. Micro-organisms that are ‘free living’ can and do fix nitrogen and provide it to plants for their usage. The rates are difficult to estimate, but have been recently estimated at between 1-5 kg N/ha/y.
Atmospheric DepositionSynthetic fertilizer usage and nitrogen oxides from fossil fuel combustion are deposited (either as ammonium or dissolved nitrates, here only showing nitrates). The amounts can reach about 40 kg N/ha/y close to heavily populated areas but falls away to closer to 1-5 kg N/ha/y in the wilderness, with agricultural areas being somewhere in between.
Lightning discharge forms nitrogen oxides NOx, which is then deposited as nitrates . This is however mostly concentrated in the tropics, and is proportional to the number of lightning strikes. It would not exceed 4 kg N/ha/y in the tropics, and probably is significantly less than 1 kg N/ha/y in temperate regions. It’s not really an important source of nitrogen, but it’s included here for completeness.
Human / Animal excretion Most forest gardeners will live in or close to their forest gardens, and when their urine and faeces (compost this properly!) are added back to the ecosystem this represents an internal flow. A single pee will add about 5.6g of nitrogen - three a day for a year will add up to 6kg N. Human manure (composted human poop) is about 6% nitrogen - one human can make about 150g per day, which over a year is over 3kg N per person. Decomposition is the process when dead plant (and animal) tissues are broken down into smaller pieces and simpler compounds by environmental conditions and other decomposing organisms (e.g. insects, fungi, bacteria). Harvesting Everyone enjoys picking food in a forest garden 🙂 But then what? Crop Removing If you are removing crops from your forest garden, or not re-adding excretions - then this represents a significant output of nitrogen from the local forest system. A commercial apple orchard can be outputting 30 kg N/ha/y in just the apples alone. Harvesting of biomass of rapidly growing plants could also lead to an annual output of up to 100 kg N/ha/y as well. Leaching is when dissolved nitrogen either enters the groundwater (travels too deeply underground for plant’s roots to grasp) or washes off the surface of the land.Erosion is the mechanical loss of solid nitrogen (from the soil or plant matter) after rainfall or other erosion events. The amount of nitrogen lost through these pathways is practically limited only by the amount of soluble nitrogen in the soil. In mature forest ecosystems in Europe leaching was measured up to 25 kg N/ha/y - ranging from 10% to 25% of the amount of deposited nitrogen.
Denitrification is a bacterial process that takes place most commonly in anoxic conditions in soil or groundwater (think warm, waterlogged soil full of nutrients), whereby bacteria use nitrate as a source of energy and release nitrogen back into the atmosphere. Denitrification rates are difficult to measure directly, and have consistently been underestimated by many techniques. Recent measurements placed it between 5 to 30 kg N/ha/y in forest ecosystems (which would make it the most significant loss of nitrogen for many ecosystems). Lastly, denitrification rates can vary seasonally - as the soil water content tends to be highest during late Autumn, Winter and Spring as plants are not absorbing very much nitrate at this time, and warm temperatures can be encountered. Nitrification is the conversion of ammonia to nitrite, and then nitrite to nitrate. Most nitrification occurs in aerobic conditions. The conversion to nitrate usually proceeds quite rapidly - the conversion to nitrite is usually the limiting factor. Nitrate assimilation Nitrogen assimilation rates (including ammonium) for conifer forest have been measured at approximately 120 kg N/ha/y, and grasslands at up to 300 - 400 kg N/ha/y. The rate of assimilation is affected more strongly by season changes further polewards - with deciduous trees there is little/no uptake at all from late Autumn to early Spring. Nitrate is the most important source of nitrogen for most plants. Ammonium assimilation. Plants are able to uptake ammonium directly to varying degrees. This pathway is much more important in cold climates, waterlogged soils and acidic soils (e.g. grasslands) - which tend to have much lower nitrification rates (thus less nitrate). Ammonification (also Mineralization) is the decomposition of organic nitrogen compounds into ammonium by microorganisms. This is a key limiting process for the growth of ecosystems. Ammonification peaks in early Summer. Immobilization is when mineral nitrogen is converted directly back to organic forms by microorganisms (such as when they are multiplying). This process occurs when the C:N ratio of the organic matter is greater than 30:1. Immobilization is when mineral nitrogen is converted directly back to organic forms by microorganisms (such as when they are multiplying). This process occurs when the C:N ratio of the organic matter is greater than 30:1.We’re going to keep returning to the local nitrogen cycle many times as it helps explains so many other concepts, so it’s worth becoming familiar with the different pieces and to start to view it as a system made up of parts that connect together. It’s also important to note that all of these pools and flows vary depending on practically every variable (e.g. temperature, water availability, day length, soil profile, pH, micronutrient balances, C:N ratio, existing plant communities, etc.) imaginable. The cycle shown above also doesn’t include all flows – some of which may be quite important (e.g. some plants have the ability to uptake organic nitrogen directly, small amounts of ammonium can be directly volatilized into the atmosphere, etc.).
Hopefully the above diagram gives you a clearer understanding of how the various flows and pools of nitrogen connect together to make up the local nitrogen cycle. What we want to understand next is – how do these flows and pools behave as a whole system? What happens if we reduce, of increase the flow of nitrogen from one pool to another? What happens if we’re manually intervening in the nitrogen flows (i.e. heavy pruning, chopping and dropping)? Where are we losing our nitrogen to (and hence less yields)?
We can’t really answer these questions exactly. But we can get a pretty accurate big picture idea of how things work in order to make better decisions. We’ve put together a simplified model simulation of the local nitrogen cycle of a forest garden. It only contains the largest input (nitrogen fixation), the largest output (denitrification – which is true under many conditions – but if it’s leaching it doesn’t really change that it’s a loss of nitrate), and the most important feedback loop (ammonification -> nitrification -> assimilation -> decomposition). The model makes basic assumptions about what is the limiting factor for the flow rate (e.g. that sunlight/warmth is the limiting factor for nitrogen fixation, the amount of plants is the limiting factor for how much nitrates they can absorb). This is enough complexity to draw some new conclusions from without getting stuck into details.
Initial Amounts
Initial Rates
- What happens to bare subsoil when the nitrogen fixing rate is high, versus low?
- What happens in a young forest when the denitrification rate is high, versus low?
- What happens to a young forest if you keep mulching all the plants?
- Once the amount of growing plants exceeds a certain amount, excess nitrate barely leaves the system – before that point, a lot is getting lost. It really is important for us as gardeners to gain sufficient plant cover, as soon as possible and to avoid bare soil.
- The different pools work somewhat separately – e.g. nitrate can be produced when plants don’t need it.
- Isn’t there some way we can slow down denitrification – it’s taking away all the nitrogen. Well… this will be an important future topic. 🙂
Well that’s about it for this article. I hope you learned something, I definitely did writing it! If you found anything interesting, or have any questions about nitrogen cycling or the model simulation – please leave in the comments
References
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Excellent! Thanks 🙂
I have added tagaste (tree lucerne) as it is NItrogen fixing. In March I ordered a truckload of mulch and have turned my backyard from a small orchard into a Food Forest.
Awesome! Tagasaste can do pretty well as a nitrogen fixer, but also worth trying some alders as they can fix more nitrogen – and they use a different type of bacteria so work in slightly different conditions. Looking forward to seeing how the food forest goes 🙂