Step 1: Understanding the Question:
The question requires evaluating the functional and technical characteristics of a tensiometer, a key instrument for measuring soil water status.
Detailed Explanation:
• Statement A (True):
A tensiometer directly measures the matric potential (or tension) of soil water.
It consists of a water-filled tube with a porous ceramic cup at the bottom. The vacuum gauge at the top reads the tension exerted by the soil matrix to pull water out of the cup.
• Statement B (True):
Tensiometers are favored in the field because they are inexpensive, do not require complex electronics, and provide real-time readings.
They are excellent for "scheduling irrigation" because they tell the farmer exactly how hard the roots must work to get water.
• Statement C (Incorrect):
Soil water flux (the rate of water movement) is typically measured using Darcy's law and requires measuring the gradient of potential between two points, or using specific flux meters. A single tensiometer only measures potential at one spot.
• Statement D (True):
Standard tensiometers only work between $0$ and $0.85$ bars. Beyond this, water inside the tube cavitates (boils/bubbles), and the vacuum is lost.
Specially designed "osmotic" tensiometers or those with modified cup air-entry values can be used to extend the range slightly, though they are less common in standard agriculture.
Step 2: Final Answer:
Statements A, B, and D accurately describe the characteristics and limitations of the tensiometer.