# Why sample in ecology? Random sampling. Practical support sheet Ecological sampling. Using a grid. 4 of 8 Student

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1 4 of 8 Student Practical support sheet Ecological sampling Why sample in ecology? In an ideal world when investigating, say, the number of dandelions in two meadows, you would count every single dandelion in each. The problem is that this might take forever and become very, very boring. So, instead, you need to take a sample. You might estimate the number of dandelions in each meadow by counting the number in several small areas and then multiplying up to calculate a value for each meadow. The idea is to maximise the usefulness of your data while minimising the effort required to collect them. Random sampling Frequently, ecologists notice a distinct pattern that may be related to one or more factors at two sites. For example, the vegetation in one field may be very different to that in another field, or the species found under oak trees may be different to those under ash trees, or the species upstream and downstream of an outflow pipe discharging into a river may seem to differ. To make valid comparisons, samples need to be taken from both sites. If the investigator chooses where to sample, the sample will be subjective. Random sampling allows an unbiased sample to be taken. Using a grid In a habitat, such as a meadow or heathland, tape measures put on the ground at right-angles to each other can be used to mark out a sampling area (Figure 1). Using a pair of random numbers you can locate a position within the sampling area to collect your data. The random numbers can be pulled from a set of numbers in a hat, come from random number tables, or be generated by a calculator or computer. The two numbers are used as coordinates to locate a sampling position within the area. The first random number gives the position on the first tape and the second random number gives the position on the second tape. Tape measure position of 0.25 m 2 quadrat using random numbers 2, Tape measure 1 Figure 1 Using measuring tapes to define a sample area. 26

3 6 of 8 Student metal spike (such as a tent peg) inserted in ground holes knitting needle multiple hit Figure 2 A point quadrat frame. Each plant species touched by the needle is recorded. Methods of measuring abundance Density Count the number of individuals in several quadrats and take the mean to give number per unit area, for example per metre squared (m 22 ). In many plant species (e.g. grasses) it is very difficult to distinguish individual plants, so measuring density is not possible. Frequency Frequency is the number or percentage of sampling units in which a particular species occurs. This avoids having to count the number of individuals. If clover was recorded in 10 of the 25 squares that make up a 0.25 m 2 quadrat frame, the percentage frequency would be 40%. You need to be consistent when determining presence or absence in a sampling unit. For example, you might decide that only plants rooted in the square are counted, or you might decide that any plant or animal in the quadrat is counted including any that touch or overhang the quadrat. Percentage cover This is the percentage of the ground covered by a species within the sampling unit. Count the number of squares within the quadrat that the plant completely covers, then count those that are only partly covered and estimate the total number of full squares that would be completely covered by that species. Estimating animal populations Quadrats cannot be used for mobile animals as these don t stay in the quadrats. A variety of different nets and traps need to be used. Animals that occur on the soil surface may be sampled using a pitfall trap (Figure 3). Those in vegetation can be sampled using a pooter directly or indirectly (after being knocked from the vegetation onto a white sheet). Insects and other small invertebrates found in leaf litter can be collected using a Tullgren funnel. Mark release methods can also be used. 28

4 Student 7 of 8 Pitfall trap for sampling arthropods jam jar sunk into soil bait of meat or ripe fruit flat stone prevents rainfall filling trap stick support ground slopes away from trap for drainage Tullgren funnel for collecting organisms from the soil or leaf litter soil sample 25 W bulb 16 mesh flour sieve Pooter for collecting insects air and arthropods drawn into tube glass collecting tube clear plastic tube Organisms move away from the heat and light, falling into the jar. glass mouthpiece polythene funnel 80% alcohol cork or rubber bung specimen tube where arthropods collect gauze covering tube opening air sucked through mouthpiece Alternatively a muslin bag of soil surrounded by water can be used to collect living organisms. This is a Baermann funnel. Sweep net rod for supporting bag 60 W bulb This net is swept through low-growing vegetation, collecting any animals in the mesh net. water soil sample in muslin bag glass funnel rubber tubing clip beaker Figure 3 Net and traps for sampling animals. 29

5 8 of 8 Student Measuring abiotic factors when sampling the environment Angle of slope Use a clinometer. Aspect Use a compass. Temperature Use a thermometer or temperature probe, but be aware that the time of day can influence the values obtained, as will cloud cover. The thermometer or probe should be placed in the same position each time a measurement is made to allow valid comparison of measurements. Light Use a light meter. Light readings can vary widely with time of day and cloud cover. It is better to take all measurements over a short period or take regular readings over extended periods using a datalogger. Oxygen concentration In aquatic systems, oxygen probes can be used to measure oxygen concentration. Humidity Relative humidity can be measured using a whirling hygrometer. It needs to be spun for 60 seconds just above the vegetation before readings are taken from the wet and dry thermometer and used to determine the humidity from a calibration scale. Conductivity The ability of a water sample to carry an electric current gives a measure of the dissolved mineral salts. The conductivity of pure water is zero; increasing ion concentration raises the conductivity. Soil water A sample of soil is dried at 110 ºC until there is no further loss in mass. The % soil moisture can be calculated using the equation: % soil moisture 5 mass of fresh soil 2 mass of dry soil mass of fresh soil Soil organic matter A dry soil sample of known mass is heated in a crucible for 15 minutes to burn off all the organic matter. The mass is re-measured after the soil sample has cooled. The % soil organic matter is calculated using the equation: mass of dry soil 2 mass of burnt soil % organic matter in soil mass of dry soil ph Universal Indicator or a ph meter can be used to test ph after mixing a soil sample with water. If using Universal indicator in the field, it is best to use a proper soil testing kit that contains some long glass tubes, with lines engraved on the sides, to show levels for adding soil and chemicals. First, 1 cm 3 of soil is shaken with distilled water before adding one spatula of barium sulphate (low hazard). This helps to flocculate (settle) the clay fraction, which is important as clay particles are very small and will otherwise cloud the water for days. Then 1 cm 3 of ph indicator solution is added and the ph recorded after the contents of the tubes have been allowed to settle. 30

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