These grassy areas are generally quite small. Boundary fences, buildings, hedges, trees and shrubs may affect the whole area, making the environment more sheltered and less varied.
However variation in the plant community may still occur however, for example due to the presence of trees or shrubs. There may also be trampled areas where people sit or children play and where trackways lead across the grass. Street lights may have an effect, particularly in urban squares.
The area of grass is often extensive and you may see differences due to variation in climatic conditions. Open areas will be much more exposed to extremes of climatic conditions than areas sheltered by boundary fences, hedges or buildings.
![]() A school playing field showing an exposed open area and a sheltered boundary |
![]() A trampled area around the goalmouth of a football pitch |
Isolated trees affect local climatic and soil conditions, but may also form a focal point where people gather, so changes in soil conditions due to trampling may be a factor. On playing pitches there is also often variation in the amounts of trampling.
It is possible to plan a fieldwork investigation which compares the plant communities between two or more different areas of grassland or along an environmental gradient. The tables below describe those abiotic (non-living) factors that are reasonably easy to measure and that may be affected by the differences discussed above. Remember that:
The effects of abiotic (non-living) factors are of course closely linked to biotic factors, in particular to human management and activity. Click for more information about the influence of these biotic factors, in particular mowing and trampling.
| Factor | What to measure | Variation due to: |
|---|---|---|
| Water content Directly affects plant growth and other biological soil processes e.g. decomposition |
Field moisture content The total soil moisture at a given moment. Some of this water drains away as soil dries and is not available to plants but measurement can provide useful comparative data |
Changes in soil structure, climatic conditions, artificial irrigation and vegetation cover |
| Infiltration rate : the rate at which water enters the soil |
Changes in soil structure, soil water content and vegetation cover | |
| Soil depth | Distance from the soil surface to the bedrock below: only useful on shallow soils e.g. on chalk | Factors that cause compaction e.g. mechanical rolling and trampling |
| Soil penetration | The depth penetrated by a weighted pin, dropped from a set height | |
| Soil pH Directly affects plant growth as well as the availability of mineral salts |
Acidity or alkalinity of the soil: small differences can be important to plants but may be difficult to detect without sophisticated equipment | Use of chemicals, e.g. fertilisers; use of materials e.g. limestone chippings for pathways; closeness to bonfire sites |
Factor |
What to measure |
Causes of variation: |
|---|---|---|
| Light: directly affects plant growth but also temperature and relative humidity | Data can be difficult to interpret (see Comparing shaded and unshaded woodland) Also considering measuring: - amount of shade - under trees - canopy cover |
Prevailing weather conditions The closeness of trees and other plants, buildings, street lamps and other human artefacts ![]() Moss growing on a lawn, shaded by trees and buildings. Is relative humidity high here? |
| Rainfall: affects soil moisture and relative humidity | Amount of rain over a set period of time. Long term data particularly useful | |
| Temperature: influences plant growth directly, also affects relative humidity | Air temperature. Long term data most useful Maximum and minimum temperatures often |
|
| Relative humidity: Particularly important to plants such as algae, mosses and liverworts. | Relative humidity of air: consider microhabitat measurements | |
| Wind: affects temperature and relative humidity. May cause direct physical damage to plants | Wind speed Wind direction |
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