Exhibition · Das Blut der Erde · The Blood of the Earth

A tree turns water into a connection between earth and sky.

Water carries minerals through roots, rises through wood, supports leaves and returns to the air as vapour. A tree is a living organism built around this moving column — and part of the watershed's infrastructure.

Schauberger called water the blood of the Earth, extending the language of circulation and health to rivers, springs and forests. Here, “living water” is that historical ecological metaphor. Water itself is not an organism; the life it supports depends on its chemistry, surroundings and movement.

The tree: a water column with living controls

In tall redwoods, water travels more than a hundred metres from roots to crown. The hydraulic limits studied by Koch and colleagues show why height matters: gravity and resistance along the route make supplying the highest leaves increasingly difficult.

SOIL → TREE → ATMOSPHERE

A water column inside a living watershed

Water rises from roots through sapwood and leaves, then returns to the atmosphere Blue continuous paths show soil-water uptake into fine roots, upward xylem transport in the outer sapwood, and delivery through branches to leaves. Transpiration releases water vapour. The central heartwood is support, not the main conducting pipe. Separate gold arrows represent phloem sugar transport from sources to sinks. Rain intercepted by leaves can evaporate or drip to soil. energy for evaporation 3 · Transpiration2 · Xylem1 · Root uptakeRain interception conducting sapwoodfine roots + root hairsdrips + infiltrationgold: phloemsource → sink
Water markers rise through the xylem.

Narrowing the pores reduces the illustrated flow. This is a qualitative comparison, not a measurement of a real tree.

Blue paths remain continuous while markers trace soil → fine roots → sapwood → branches → leaf veins. Pale markers outside leaves represent vapour, not liquid droplets. This is a simplified daylight transpiration stream: water cohesion, xylem structure and a soil-to-air water-potential gradient explain the ascent. Branches, roots and tissue layers are schematic; marker speed is illustrative. USGS: transpiration · UC ANR: tree anatomy.
SOIL → ROOT → XYLEM → LEAF → AIR

Evaporation supplies the pull

The main driver is cohesion–tension. Evaporation from moist leaf cell walls lowers leaf water potential and creates tension in the xylem. Cohesion between water molecules transmits that pull through water-filled conduits; adhesion helps maintain contact with their walls. Water moves along a water-potential gradient, generally from wetter soil towards the much drier atmosphere. Plant transport explained ↗

Capillarity contributes at small scales, but cannot explain a tall tree by itself. The flow also depends on hydraulic resistance and the supply of soil moisture. There is no mechanical pump in the trunk: the tree grows and maintains the conduits, and regulates loss through its leaves.

Read the tree from the ground upwards

Fine roots and root hairs provide absorbing surface. Water crosses outer tissues towards the vascular system; at the endodermis, the Casparian strip restricts the route between cells, bringing uptake under membrane control. This is a selective biological boundary, rather than a guarantee that every contaminant is excluded. Root anatomy ↗

The routes and controls in a woody tree
PartIts role
Fine roots & root hairsAbsorb soil water and dissolved nutrients. Larger roots anchor the tree and carry the supply onwards.
Xylem & sapwoodXylem conducts water and minerals. Its active outer wood, the sapwood, carries the upward flow and also stores water.
HeartwoodOlder central wood provides support; it is not the main conducting route.
Vascular cambiumThe growth layer makes new xylem inward and new phloem outward.
PhloemTransports sugars from producing tissues to growing or storing tissues. Source-to-sink flow may travel up or down.
Outer barkProtects the tissues beneath it.
Leaf mesophyllMoist internal surfaces where water evaporates into the leaf's air spaces.
Stomata & guard cellsPores and their living controls regulate gas exchange and water-vapour loss.

Anatomy: Iowa State University Extension; transport and leaf controls: OpenStax Biology; internal water storage: Čermák and colleagues, 2007.

THE HYDRAULIC LIMIT

Drought makes the column vulnerable

As soil dries or the air's demand rises, tension can become harder to sustain. Cavitation can create gas bubbles; an embolism blocks a conducting pathway. Closing stomata conserves water, but also limits carbon-dioxide entry for photosynthesis. This trade-off links tree growth, heat and drought to its hydraulic system. Stomatal safety and efficiency, 2019 ↗

A tree's plumbing reaches beyond its trunk

A tree changes what happens to rain before it reaches a drain or stream. Its canopy, roots, surrounding soil and atmosphere work together; their effects depend on the site.

CANOPY

Intercept and delay

Leaves and branches temporarily hold rainfall. Some evaporates; some reaches the ground as throughfall or runs down the stem. A paired-catchment study in Wisconsin measured reduced stormwater runoff where street-tree canopy was retained.

SOIL

Keep room for infiltration

Root channels and leaf litter help create conditions for rain to soak into soil. Compaction and paving interrupt that system. Infiltration replenishes soil moisture and may feed groundwater; the route depends on soil, geology and saturation. EPA: stormwater and street trees ↗

ATMOSPHERE

Return water and cool

Transpiration transfers liquid water from soil to atmospheric vapour. Evaporation uses energy, helping cool leaves. Weather, species, leaf area and soil moisture control the rate. This is part of evapotranspiration, which also includes evaporation from soil and other surfaces. USGS water cycle ↗

Protecting a forest and increasing streamflow are different goals. Trees use water, so forest planting can reduce water yield even while providing shade, habitat and erosion control. A global analysis of forest management found that landscape storage and evapotranspiration help explain the response. Climate, soils, forest age, disturbance and timescale matter; there is no universal “more trees means more water” rule.

Water inside living tissues: local environments matter

In cells, water surrounds ions, proteins and membranes. Near a biological surface, its interactions and mobility can differ from those of water farther away. These hydration layers are dynamic environments, not permanent crystalline shells or a new kind of H₂O.

LOCAL CONTACTS · DYNAMIC HYDRATION

Water meets living surfaces

Local hydration near proteins, membranes and the vascular glycocalyx A cell contains proteins and organelles, surrounded by water that exchanges at their surfaces. A blood vessel has an endothelial lining and a glycocalyx brush. Blue water symbols mark local contacts without representing a fixed or uniformly aligned phase. Red blood cells move through the lumen under circulatory pressure. Cell waterVessel lumen contacts with proteins + membranesendothelium + glycocalyxhydration shells exchange continuouslyblood flow: circulatory pressure
Schematic molecular motion; not to scale.
Blue symbols highlight local hydration contacts, while faint symbols mark surrounding water. Neither colour gives a measured fraction, and the symbols do not imply uniform crystalline ordering. Water exchanges near membranes and proteins; surface chemistry changes its local structure and dynamics. The vascular glycocalyx is a real protective surface layer. A universal charged "exclusion-zone battery" powering vessels is a separate hypothesis discussed in The Fourth Phase.
MEASURED IN CELLS

Local change, rather than universal order

A 2024 Raman study by Lang and colleagues found about 3% non-bulk-like water in three examined cell types. That population had a weaker, more disordered hydrogen-bond network; most measured water was bulk-like. The result is specific to those cells and that measurement, but it directly challenges the claim that most cellular water forms highly ordered layers.

AT THE VESSEL WALL

A living surface that responds to flow

The glycocalyx is a hydrated, sugar-rich coating on endothelial cells. It participates in the vessel's barrier and response to shear stress. Experiments in cultured endothelial cells showed its organisation changing under flow. That established biology does not demonstrate an exclusion-zone battery powering circulation.

A RELATED QUESTION

What changes at an interface?

The Fourth Phase exhibit examines exclusion-zone experiments and the competing interpretations of them. Hydration near biomolecules, particle exclusion near a laboratory surface and a proposed extra thermodynamic phase are distinct questions. The Molecule exhibit supplies the underlying polarity and hydrogen-bond chemistry.

The biography of a drop, made measurable

Schauberger's language of birth, maturity and exhaustion gives water a story. Modern hydrology follows a more testable history: where it fell, how long it travelled, what dissolved in it, which organisms it encountered and where it will go next. Rain, groundwater, sap and blood belong to connected cycles, but each has a different composition and biological setting.

Protect that history through the watershed: preserve root zones, limit soil compaction, keep contaminants out of recharge areas and assess water quality through measurements. A spring's clarity, coolness or movement does not establish drinking safety. Those practical questions continue in The Hunger of Water and The Poisoned Aquifer.

Established

Plant anatomy, water-potential gradients and cohesion–tension explain a tree's hydraulic transport. Hydration environments influence biological interactions.

Historical framing

“Blood of the Earth” asks us to think about circulation, catchments and ecological health. It is a metaphor for stewardship.

Not established

Literal life in water, durable biological “imprints” in vapour and extraordinary energy from a drop are not demonstrated by the transport shown here.

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