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Water Monitoring Equipment - general.

Water monitoring equipment

 

Water monitoring Devices: these are many and varied - they do not all do what they are expected to do! You cannot beat good agronomic knowledge and advice - do not be persuaded by the plausable salesman - talk to people with experience. If you put 20 different devices in the soil you may well get 20 different suggestions - they are not all right!

The 'right' equipment used badly is no better than bad equipment. ' An essential tool is the Spade, to be kept at all times in the truck! Even if you have the best water monitoring system in the world (see later), you need to check whether the information you have collected applies to the whole field or just those particular spots. Also, when your monitoring system tells you something you do not understand it is important to go to the field, maybe with your adviser, and dig - you will learn a great deal.

Computer Models: Are all based on the Pennman-Monteith equation, which takes weather data and calculates evapotranspiration rates for crops by adding crop factors, based on crop cover, stage, soil type etc. Much better than nothing as at least they make the grower think! Are as accurate as the information supplied! But, it is not easy to identify when a 'soil is Full' or what percentage of water pumped is actually getting into the soil as needed. When used in conjunction with good point measurement they can be useful.

Gypsum blocks, TDR's, and other buried devices: These can be useful, but need to be installed very carefully (water can run down the cables and by digging holes to install, the soil structure can be changed, giving misleading data). You need to know what volume of soil they are measuring, whether this is useful or misleading and whether they are actually accurate - some most definitely are not!

Tensiometers: These come in various forms - basic, quick draw, electronic etc. They all work on the same principle - measuring the 'suck' (usually in Kilopascals) required to take water from the soil as a plant may do. When used by scientists they can give useful information, but most farmers find them confusing and often misleading.

As can be seen from Tensiometer graphs, the 'moisture' reading follows an exponential curve and once one gets above 30kp there is very little change. Identifying when to water is not clear. Soil structure will effect the readings and generally it is found that they tend to over estimate both dry and wet. A scientist will tell you that you should water every time you get to 30 or 40 or 50 or 60 depending on the 'expert', but it is very difficult to know. Most people will be watering too soon to get maximum water use from the soil water that is 'free', hence wasting water. There are quite a few situations where water use increases as the soil dries, probably due to increases in oxygen, so watering too soon will prevent this. When you need to 'see' what is happening at multiple depths, they become more confusing as they are difficult to install in one plane, which is important. Better than nothing, but not ideal. Speak to a 'real expert'.

Neutron Probes - only portable: Are considered a standard around the world. They measure using a radioactive source, at multiple depths and in deep soils with cheap labour are very successful. However, here in the UK they are operated by companies that come round once, or occasionally more, per week, collect the data, interpret it and make recommendations. But there are a few drawbacks: - Multiple sites become expensive. -Not too good near the soil surface. -Measure a large volume of soil - can be good and sometimes not so good. -The volume of soil measured can vary according to the amount of water in the soil. -By measuring large volumes of soil, can average wet and dry, which will miss the true picture. -Complicated to own, due to regulations.

Capacitance Probes - permanent or portable: These measure electronically, through plastic tubes inserted in the soil, to multiple depths and can be logged to monitor continuously. But, beware, some are very good and some not so good! Some are very accurate and some very inaccurate - check 'scientific accreditation' and also with anyone who has been using them for some time. Check sphere of influence (some are little better than tensiometers, which rely on touch

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