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Groundwater Archives - Page 2 of 2 - STS Switzerland (EN)
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Water in spite of drought

Water in spite of drought

Water management experts at the Karlsruhe Institute of Technology (KIT) have constructed a subterranean dam with an integrated hydroelectric plant inside a karst cavern on the Indonesian island of Java. The power station located 100m below ground now provides plentiful water from the cavern during the dry season. Two data loggers installed there measure the water levels both in front of and behind the dam wall. The level of the upper water reaches 15 – 20m, while the lower level, where water discharges again from the turbine, attains a maximum of 2m.

The karst area of Gunung Kidul on the south coast of Java is one of the poorest regions in Indonesia. The ground is too barren for a bountiful supply and in the dry season the flowing waters actually run dry. Water from the rainy season peters out quite quickly, but does collect within an underground cave system. This natural water reservoir has now been harnessed with a cave power station. The fact that even in the dry season over 1,000 liters of water per second flows through the Bribin Cave speaks for the ideal location of this dam. Instead of complex turbines, the mechanical energy to drive the feed pumps is generated by reverse-driven circulation pumps. The five parallel-operating feed pumps are thus highly cost-effective, incurring only minor operating and maintenance costs. The supply pumps send part of the water 220m high to a lake named Kaligoro Reservoir situated upon a mountain. The key stumbling block to this project was successfully overcome during the test damming phase. The cave did effectively hold the water and a crucial dam height of 15m was indeed achieved.

In March 2010, the installation was then handed over to the Indonesian authorities. It can now provide 80,000 people with up to 70 liters of water per day. Previously, the populace had only 5 – 10 liters available per day during the dry season, for personal hygiene, household and livestock purposes. Incidentally, each German uses on average 120 liters per day, for comparison.

Function of the pressure data loggers

The pressure loggers measure the water levels in front of and behind the dam wall. The normal level amounts to 15m, but it can reach up to 20m during heavy rainfall. The other probes measure the water level whilst submerged, in particular where water discharges from the turbine. Levels of up to 2m are recorded in this area. The pressure loggers from STS were chosen due to their high overload capacity of 3x their full-scale range, the low characteristics deviation of maximal 0.1% and an enhanced long-term stability of between 0.1 % und 0.5 % FS per annum.

These level loggers cover pressure ranges between 0 – 100 mbar and 0 – 600 bar, thus permitting level measurements in the ranges of 0 – 100 cmAq to 0 – 6,000 mAq. The measurement interval itself is variable between 0.5s and 24h. The units are further distinguished by a measurement data memory of up to 1.5 million measured values and a narrow probe diameter. Additionally, their standard lithium batteries can be swapped out on site in no time at all.

Variable data-saving intervals dependent upon pressure or time permit for flexible measurements. With the use of various materials like stainless steel, titanium, PUR, PE or Teflon cable, a high medium tolerance is achieved, allowing for the most varied of applications. Besides the level recordings of groundwater, wells, boreholes, lakes and rivers, these level loggers are also suited to leak testing in gas, water and other pipeline projects, as well as pipeline analysis and pressure testing in gas, water and community heating pipeline networks. They have also proven themselves optimally in gas pressure control stations and in the verification of a constant supply pressure.

Sources: Karlsruhe Institute of Technology (KIT) – Institute for Water and River Basin Management (IWG)

Hydrostatic pressure measurement with piezoresistive level sensors

Hydrostatic pressure measurement with piezoresistive level sensors

Whether as a life-giver, a danger to life or simply a refreshment in summertime, the element of water determines daily life on earth in many ways. Because of its sheer importance, a reliable monitoring of this element becomes essential.

What cannot be measured can also not be managed efficiently. From fresh water supply, drinking water treatment, storage and consumption measurement, to waste water treatment and hydrometry, it will not be possible to work and plan efficiently without the correct input parameters. A range of devices and processes are now available to capture today’s complex hydrometric infrastructure. The classic in water level measurement is without doubt the level gauge, for which an accuracy of +/- 1 cm must be applied and which, of course, still functions completely “analog” – having to be inspected visually and doing without electronic data transmission. Today, far more advanced and precise instruments provide remote transmission of the measured data, including piezoresistive pressure sensors for water level measurement in both groundwater and surface waters.

Level measurement with pressure sensors

Pressure sensors for level measurement are installed at the bottom of the water body to be monitored. In contrast to level gauges, it is generally not possible to read them without getting wet. This is not necessary either, since piezoresistive level sensors were developed to meet today’s requirements for process automation and control. It goes without saying that water levels can thus be measured without human intervention, which makes continuous monitoring at difficult-to-access locations possible in the first place.

Hydrostatic level sensors measure the hydrostatic pressure at the bottom of the water body, where the hydrostatic pressure remains proportional to the height of the liquid column. Additionally, it is dependent upon the density of the liquid and gravitational force. According to Pascal’s law, this results in the following calculation formula:

p(h) = ρ * g * h + p0

p(h) = hydrostatic pressure
ρ = density of the liquid
g = gravitational force
h = height of the liquid column

Important considerations for trouble-free level monitoring

Because piezoresistive level sensors are placed at the bottom of the water body, they are then protected from surface influences. Neither foam nor flotsam can now influence the measurements. But, of course, they do have to be adapted to the expected underwater conditions. For salt water, for example, a level sensor with a titanium housing is to be preferred. Should galvanic effects be expected, however, then a measuring device of PVDF would be the best choice. In most freshwaters, high-quality stainless steel will be sufficient. And lastly, a sufficient grounding of the level sensors is essential to prevent damage from lightning strikes, for example (read more on this topic here).

Modern level sensors: All data from just one device

Piezoresistive level sensors can be used for level monitoring in open waters such as lakes, in groundwater occurrences and also in closed tanks. In open waters, relative pressure sensors will be used. With these devices, air pressure compensation is provided by a capillary inside the pressure sensor cable. A differential pressure sensor is normally used in tanks, since the gas overlay pressing down on the liquid must also be taken into account (read more on this topic here).

Because piezoresistive level sensors are largely self-sufficient and can also be optimized for very high pressures, measurements at great depths now become a possibility. Theoretically, there are hardly any limits to this depth, only that the pressure sensor cable has to be long enough.

Figure 1: Examples of level sensors for hydrostatic pressure measurement

Apart from the fact that there are hardly any depth limits, these modern measuring instruments are also extremely versatile. After all, it is not only the level of a water body that is of interest to us. Water quality is also of great importance for groundwater monitoring. The purity of a groundwater reservoir, for example, can also be determined by its conductivity, where the lower the conductivity, the purer the water will be (read more about conductivity here). In addition to conductivity sensors, level probes today are now also available with integrated temperature measurement. Piezoresistive level sensors provide a wide range of monitoring tasks and are without question preferable to the level gauge in most cases.

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