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Closing the cycles

Energy: The Flow That Drives Everything

Terra Humana editorial teamLast updated: 2026-10-1410 min read

Morning sunlight falls through several layers of leaves onto covered ground on a Mediterranean slope

In brief

The one-way path of sunlight through leaves, plants, animals and soil life until it leaves as heat. Energy does not circle; it drives every cycle that does.

How energy flows through the land

The honest first sentence about energy is that it does not circle. Water falls, soaks in, rises as vapour and falls again. Nitrogen passes from a leaf to the soil and back into a root. Energy makes only one journey. It arrives as sunlight, is captured in leaves, stored for a while in sugar, wood, seed, flesh and humus, and leaves as heat every time something grows, moves, breathes or rots. What drives the other cycles of a landscape is this steady stream from the sun. Without it no water would be lifted by a plant and no nutrient freed by a fungus.

The capture happens in the leaf. Zhu, Long and Ort calculated that photosynthesis can at best turn about 4.6 percent of the solar energy reaching a leaf into biomass in most plants and about 6 percent in plants with the C4 pathway, such as maize and many tropical grasses. Over a whole season in the field, even the best crops measured reach only about half of these ceilings. Small as that sounds, it feeds almost all life on land: Field and colleagues estimated that plants fix about 105 billion tonnes of carbon a year, a little more than half of it on land.

From there the energy is passed on and spent at each step. Raymond Lindeman's study of 1942 laid the ground for the rule of thumb that only about a tenth of the energy at one level of a food chain reaches the next; the rest goes on breathing, moving and staying warm. The figure is an average, not a law, but its message holds. On land the largest consumer is usually not the deer or the goat but the soil. In forests, a compilation by Cebrian found, herbivores eat only a small share of the yearly plant growth. The rest falls as leaves, twigs and dead roots and feeds the fungi, bacteria, mites and worms that break it down.

Plants also feed the soil directly. Part of the sugar they make goes down into roots, into the fungi around them and into the root zone as exudates. In a review of labelling studies, Pausch and Kuzyakov found that grasses, most of them perennial, send about one and a half times as much of their assimilated carbon below ground as annual crops do. This underground payment is what keeps the soil food web working, and with it the nutrient cycle.

The energy flow

Tap a station to see the techniques that close the cycle there.

Catch sunlight, feed the soil
Sunlighton leavesPlant growthRootsand fungiAnimalsLitter andpruningsSoil lifeHumusand charHeat andcooling

Where ordinary land use wastes it

The usual way of farming loses energy in three ways.

Sunlight falls on bare ground. A field that lies ploughed and empty for half the year captures nothing during that time. The light that a green cover would have turned into sugar heats the soil instead, dries it out and, on a Mediterranean summer slope, leaves it hot enough to harm the life within it. A single-layer orchard over bare soil uses one floor of a building that could have several.

The stored energy is burned or hauled away. Prunings, straw and crop residues hold the energy that the soil life needs. Where they are burned, that energy is released in minutes as heat and smoke. Where they are carted off, it leaves the land for good. The soil goes hungry, its life thins out, and with it go the humus and the crumb structure that hold water and nutrients.

Fossil energy fills the gap. Industrial farming replaces much of the work the sun and the soil life used to do with energy from oil and gas. An FAO paper estimated the energy used along the whole food chain, from making fertiliser to cooking, at about 95 exajoules a year, roughly 30 percent of the world's energy use. Nitrogen fertiliser alone is costly: according to the International Energy Agency, ammonia production accounts for around 2 percent of total final energy consumption, almost all of it from fossil fuels. A farm that depends on this subsidy is not running on its own sunlight.

Techniques that catch more sun and keep it in the land

Behind all of them is a simple aim: more leaves for more months, and everything that grows returned to the soil life rather than burned. Bill Mollison's design method starts with the same questions: where the sun comes from, where the wind blows from and how the slope falls. The cycle graphic above shows which technique works at which station.

Sunlight on leaves. A cover crop and a living mulch keep the ground green through the cool, wet months, when a bare field captures nothing. Polyculture mixes plants of different heights and seasons so that one is growing while another rests. Pioneer plants close a bare surface fastest and make it habitable for what follows.

Plant growth. A food forest and agroforestry stack several layers of leaves above one patch of ground. Syntropic agriculture arranges plants by their light needs and their place in succession and prunes them hard, so that the system keeps producing new growth. Biomass plants are grown only to be cut, and a plant guild groups species so that each fills a gap the others leave.

Roots and fungi. Mycorrhiza receives sugar from the plant and pays for it with water and phosphorus from pores no root can reach. Rhizobia in the root nodules of nitrogen-fixing plants also live on the plant's sugar and use its energy to bind nitrogen from the air. Both are energy from the leaf put to work underground.

Animals. In silvopasture animals graze between trees and turn plants the soil cannot use directly into dung, which feeds the soil life on the spot.

Litter and prunings. Mulch and sheet mulching lay the stored energy of cut plants on the soil surface, where worms and fungi can reach it. In a compost heap the same material is broken down in one place; the warmth in its core is the energy of the plants being released, and what remains feeds the soil life. Green manure grows that food for the soil in one season, and Hügelkultur buries wood that feeds the soil slowly for years.

Soil life. The soil food web is the largest consumer on most land and the engine of the nutrient cycle. Fed well, it builds a stable soil structure with its own sticky by-products.

Humus and char. Humus is energy and carbon held in the soil for years to decades. Biochar keeps part of the carbon of prunings far longer than mulch would, and terra preta shows what centuries of returning ash, charcoal and waste can build.

Heat and cooling. The regreening of dry land turns sunlight that would only heat bare soil back into transpiration, which cools. Nurse trees shade young plants and the ground beneath them. Where heat is welcome, stone does the opposite: a herb spiral stores the warmth of the day and releases it at night, and rock mulch protects the soil where organic cover would burn or blow away.

How it looks at Sa Medada

Sa Medada is a slope in Jerzu, in the Ogliastra on the east side of Sardinia. Sunlight is not what this land lacks. The winters are mild, and the dry season runs roughly from May to September, when the sun is strongest and the rain is absent. In summer the limit on growth is water, not light, which is why the water cycle and the energy flow are hard to separate here. An old olive grove covers part of the land, and maquis grows on the steeper slopes; the LiDAR wetness map shows a comparatively dry main area and moister channels along the edges.

Project Eden therefore starts with pioneer plants, ground cover and water retention. Seen from the energy flow, the aim is that sunlight should fall on leaves rather than on bare earth, and that what grows should stay on the land as food for the soil. A laboratory analysis of the soil does not yet exist, so we make no claims about its humus or its life.

The mild winters allow plants that need a great deal of warmth and light to grow in the open ground, among them banana, mango, avocado, papaya, passion fruit, lychee and moringa. Several fast nitrogen fixers are already in the soil, including Leucaena, Inga edulis, Tephrosia and the coral tree. Plants of this kind are cut back regularly in syntropic systems to feed the soil, and whether that can work on this slope is still open. The service tree, planted in 2024 as the first tree, stands on the very hot southern flank, where the summer sun strikes hardest.

Plants in this entry

Frequently asked

Why is energy not a cycle like water or nutrients?

Because it is used up as it works. Water and nutrients can pass through the same field again and again. Energy arrives as sunlight, is stored for a while in sugar, wood, humus and the bodies of animals, and leaves as heat each time something grows, moves or decomposes. It can only be passed on, never returned. That is why a landscape needs fresh sunlight every day, and why the energy flow matters for every other cycle: water, nutrients, carbon and seed all move only because sunlight keeps something alive and working.

How much of the sunlight do plants actually use?

Very little. Zhu, Long and Ort calculated that photosynthesis can at best turn about 4.6 percent of the solar energy reaching a leaf into biomass in plants with the common C3 pathway and about 6 percent in C4 plants such as maize. Over a whole season in the field, even the best crops measured reach only about half of these ceilings. Most land does far worse, mainly because the soil lies bare or the plants are too small for much of the year. The largest gain is therefore not a better leaf but more leaves for more months.

What is the ten percent rule?

It is a rough rule from ecology, going back to Raymond Lindeman's study of a bog lake in 1942. Only about a tenth of the energy taken in at one level of a food chain reaches the next: from plants to herbivores, from herbivores to predators. The rest is spent on breathing, moving and keeping warm, or leaves as dung and dead matter. The figure is an average and varies widely between ecosystems. It explains why there are far fewer foxes than rabbits, and why the soil life that eats the dead matter is the largest consumer on most land.

Does burning prunings and crop residues waste energy?

From the point of view of the land, yes. The energy stored in the leaves and wood was meant to feed fungi, bacteria, worms and insects in the soil, which build humus and release nutrients as they work. Burning releases that energy in minutes as heat and smoke, and with it most of the nitrogen and the organic matter. Laid down as mulch, chopped into the soil surface or turned into biochar with a cleaner process, the same material keeps working on the land for months or years.

What does energy have to do with the water cycle?

Far more of the sunlight that falls on a green landscape goes into evaporating water than into photosynthesis. Turning one litre of water into vapour takes about 2.45 megajoules, and that energy is drawn from leaves and air, which is why a planted slope stays cooler than a bare one. Where there is no water in the soil, the same sunlight heats the ground instead. Catching energy and holding water are therefore two sides of the same task, and on dry land the water usually decides how much sunlight plants can turn into growth.

Floor of a Mediterranean forest garden: leaves, freshly cut branches and decaying wood on dark crumbly soil, fungal threads and an earthwormNext in this themeThe Nutrient CycleThe path of nitrogen, phosphorus and other nutrients from air and rock through plants, animals and soil life back to the roots.

Related terms

Mentioned in

See this in practice

Permaculture principles at work here

The design principles after David Holmgren that this page puts into practice.

Sources

  • Zhu, Long and Ort, What is the maximum efficiency with which photosynthesis can convert solar energy into biomass?, Current Opinion in Biotechnology 19, pp. 153-159 (2008)
  • Ort, Zhu and Melis, Optimizing antenna size to maximize photosynthetic efficiency, Plant Physiology 155, pp. 79-85 (2011)
  • Zhu, Long and Ort, Improving photosynthetic efficiency for greater yield, Annual Review of Plant Biology 61, pp. 235-261 (2010)
  • Field, Behrenfeld, Randerson and Falkowski, Primary production of the biosphere: integrating terrestrial and oceanic components, Science 281, pp. 237-240 (1998)
  • Lindeman, The trophic-dynamic aspect of ecology, Ecology 23, pp. 399-418 (1942)
  • Cebrian, Patterns in the fate of production in plant communities, The American Naturalist 154(4), pp. 449-468 (1999)
  • Pausch and Kuzyakov, Carbon input by roots into the soil: quantification of rhizodeposition from root to ecosystem scale, Global Change Biology 24(1), pp. 1-12 (2018)
  • Allen, Pereira, Raes and Smith, Crop evapotranspiration: guidelines for computing crop water requirements, FAO Irrigation and Drainage Paper 56 (1998)
  • Sims (FAO), Energy-smart food for people and climate, Issue Paper, Food and Agriculture Organization of the United Nations (2011)
  • International Energy Agency, Ammonia Technology Roadmap: Towards more sustainable nitrogen fertiliser production (2021)
  • Bill Mollison, Permaculture: A Designers' Manual, Tagari Publications (1988)

Last updated: 2026-10-14