Environment

In environmental noise reports or technical specifications of household appliances, we often encounter the figure 50dB. But in reality, does a 50dB noise level cause discomfort or affect health?

In daily life as well as industrial production, noise is increasingly becoming a serious form of environmental pollution. It silently has negative impacts on human hearing and the nervous system.

In the transportation of temperature-sensitive goods such as food or pharmaceuticals, setting and maintaining the correct temperature is essential. Even short-term temperature deviations can alter the quality of the shipment and cause financial losses.

It's currently mid-April, the beginning of summer, and sudden rain showers or humid weather can make indoor air stuffy. Keep these tips in mind to prevent mold and mildew in your home!

The EC index reflects the amount of dissolved salts present in the soil solution. When this level changes, the nutrient status and the root's absorption capacity also change. This is why EC is often monitored throughout the cultivation process.

According to specialized literature, the electrical conductivity (EC) of soil is typically between 0.2 and 1.2 mS/cm. This is the range within which plants can absorb nutrients relatively stably. When it falls below this threshold, the amount of dissolved ions is insufficient, leading to nutrient deficiencies. When it exceeds this threshold, the salt content increases, affecting plant growth.

Electrical conductivity (EC) is a fundamental parameter in water quality assessment. This index reflects the ability of a solution to conduct electricity through dissolved ions, including metal salts and inorganic compounds such as NaCl, KCl, nitrates, or phosphates

Groundwater detectors are indispensable tools for identifying hidden underground aquifers. Thanks to their ability to analyze geological strata, these devices help users pinpoint optimal locations for both domestic and industrial water extraction

Groundwater is the amount of water that accumulates in the pores of the soil or in the cracks of bedrock beneath the surface. This water source is not a free-flowing river but usually exists in aquifers. However, groundwater does not always exist as large streams but is often hidden within complex geological structures.