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Soil moisture - Wikipedia, the free encyclopedia |
 | | Soil moisture may be measured in situ with different instrument, such as Time Domain Reflectometry (TDR), neutron probe, capacitance probe, etc. In the laboratory, it is measured gravimetrically; by weighing the moist volume of soil, drying it, and then weighing it again. |
 | | Conditions where soil is too dry to maintain reliable plant growth is referred to as agricultural drought, and is a particular focus of irrigation management. |
 | | Soil moisture is more generally considered within the context of hydrology, where it represents the immediate store of infiltrating rainfall, before it either evapotranspires or contributes to groundwater recharge. |
| en.wikipedia.org /wiki/Soil_moisture (309 words) |
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