Drainage
Poor drainage
Poor drainage can show up as puddles of surface water that can’t drain away. Excess water pushes out air in the soil, which is essential for plant growth. Soils need to be aerated to ensure oxygen is available for respiration of plant roots – otherwise the roots will die.

The time it takes water to drain away will depend on the size of the soil pores that hold the air and water.
If the pore spaces are large the water will drain fast. When they are small the water will drain slower.
For example, clay swells on wetting, the pores are closed off and water cannot move through. Where there is no air the soil water will not move to carry nutrients to the roots of plants.

The wet soil in this paddock has made germination patchy and plant growth uneven.
Good drainage
Well-drained soils are warmer and produce earlier crops in spring. They contain more soil organisms, and may increase nutrient availability.
Drainage problems

Poorly drained soils are a problem because they:
- lack air required by plants for growth and respiration. Roots of plants will be unable to carry nutrients to the plants
- cause seeds to have poor germination and uneven growth because they don’t have enough air to respire
- are slow to warm up in spring, which can slow down plant growth
- contain nitrogen that is unavailable to the plants. Plants growing in these conditions will have yellow leaves
- are difficult to cultivate which can lead to a delay in sowing and delayed harvesting dates
- are easily damaged by machinery.
All these things can combine to decrease soil fertility and crop and pasture yield.
What causes poor drainage?
- A hard pan
Iron, clay or humus can be removed (leached) by water from the upper layers of the soil and settle to form a hard layer in the subsoil. This is called a hard pan. Water will stay on this layer and not drain away. It is hard for water to drain though this layer.
- A plough pan
When machinery like ploughs and rotary hoes are used to cultivate the soil at the same depth soil particles will pack together. This compacted layer called a plough pan will stop water draining.
- Fine textured soils with poor structure
Signs of poor drainage
- In clay soils a pan will look a patchy grey/blue colour.
- Surface water, ponding and flooding.
- Yellow leaves on plants caused by a lack of nitrogen and oxygen.
- Machinery tracks.
- The soil particles pack together into clods.
- Rushes, buttercups and other weeds.
Improving drainage
Subsoiling
A compacted layer of soil can be broken up and loosened by subsoiling.

This is sometimes also called ripping or aerating. This makes space for roots, water and air. Subsoiling is expensive because of fuel and labour costs.
The water content of the soil affects the success of subsoiling. Soil that is too wet will not break up but will smear instead. Dry soil will break into coarse blocks.
The subsoiler has chisel type blades that are pulled though the soil, which lifts and cracks.
Aerator

Soil aerator machines can be useful where there is surface soil compaction. These are useful on turf and sports fields. The aerator is attached to a tractor. They can be coulters that have spikes or tines on them. The spikes or tines are punched in and out of the soil. The spikes make holes in the soil, which helps remove excess water from the soil surface. This increases root growth and improves crop yield because more air is available to the plant roots for respiration.
Artificial drainage systems
The removal of excess water from the ground surface or the root zone is called drainage.
The aim of a drainage system is to carry surface water away or to lower the water table.
Water tables
Some of the water that falls on the soil runs off but a lot of it goes into the soil through wormholes and cracks. It takes up pore spaces until it reaches rock, a hard pan, or heavy clay subsoil. The water collects and forms a waterlogged layer. The top of this layer is called the water table. The water table may be only a few centimetres from the surface or many metres down. Its depth will vary with the season.

When the water table is very high it needs to be lowered by drains.
Open drains, tile drains or plastic piping can be used to lower the water table. The type of system to use will depend on the drainage problem.
Surface drains
Machinery is used to shape the land to make somewhere for excess water to go. This is often considered a cheap option.

- Open drains or ditches
Ditches can be of any shape or size and they can take large volumes of water.
These drains do use up land and do need looking after. Excessive weeds should be cleared so they continue to work properly.
- Graded banks
These are formed using a grader or bulldozer. Sloping land is terraced so the water is allowed to flow down the slope and drain away.
Subsurface drains
These drains are formed underground. They can be:

- made of clay or plastic piping.
The pipes are laid under the soil surface. The depth and spacing of the pipes depends on the soil type. The depth of the drain is the level the soil will drain to. When trees are close to the drains their roots can grow into the tiles. This stops them working properly. Tree roots should be pruned regularly.
Mole drains

These are formed with a mole plough. A series of cracks and channels are formed using a metal plug pulled through the soil. Water can drain through these gaps. Mole drains are generally used along with tiles, and run at right angles to them. They are not permanent and need to be re-done every 5–7 years. These types of drains are not suitable on sandy soils, as the channels would collapse. They can be used on clay soils and loams.
Other methods that can be used
Raised beds
These are useful when the water table is high. The soil is raised above ground level. The soil can be raised in a structure of wood, brick, or cement blocks.
Bedding

This is sometimes referred to as humps and hollows. The idea is to shape the land into humps and hollows. Surface runoff moves into the hollows and drains away. You can see this method on flat low-lying areas such as the Hauraki Plains. This technique does not remove water from within the soil but moves water from the surface.
Key points
Poorly drained soils usually have poor aeration. They may have nutrients leached from them. Wet soils will be slow to warm up in the spring. Soils need to be aerated to ensure oxygen is available for transpiration and respiration.
Well drained soils are:
- warmer and produce earlier crops in spring
- more likely to have readily available nutrients
- better for soil organisms.
Drainage can be improved with: cultivation, adding organic matter, raising the garden or seedbed and/or providing drainage systems such as field tiles to remove excess water into waterways.
What's next?
Go to: 10 Hydroponics.