Summary edit

Definition edit

Hydraulic conductance is a measure of the efficiency of bulk flow through a material, and defined as the flow rate per unit pressure driving force.

Terminology and equations edit

Measurement of xylem hydraulic properties falls into two main categories. The first involves measuring flow rate for a given driving force, with the resulting conductance (F/DP) being normalized by the length of the segment and referenced either to the cross sectional area of the xylem (Ks: xylem-specific conductivity) or to the leaf area supported by the xylem (KL: leaf-specific conductivity): Ks = F L / (DP Asw) KL = F L/(DP AL) where F is the recorded flow rate, L is the length of the measured segment, DP is the pressure drop across the segment, Asw is the cross sectional area of the conducting sapwood, and AL is the total leaf area supplied by the measured segment. These two conductivities are inter-related by the ratio of xylem cross-sectional area to supplied leaf area, a parameter known as the ‘Huber value’, Hv: KL= HvKs.

Measurement approaches edit

For a stem segment, this can be measured by multiple methods, in the field or lab, for stem segments in vivo, or for excised stem segments

In vivo methods edit

1. Sapflow and water potential driving force

2. Transpiration and water potential driving force

When using the sapflow method for hydraulic conductance the Ks can be determined as one of several other water use and water relations traits (e.g., whole plant hydraulic conductance, whole plant water use, etc).

The transpiration method is relatively simpler, as depends on leaf-level gas exchange measurements rather than more logistically intense sapflow work.

Excised segment methods edit

1. Pipette method

2. Balance

3. Flowmeter

The balance method allows for continuous logging of flow rate and is best suited for a controlled laboratory environment. The pipette and flow meter methods are more portable and suitable for field based measurements but do not allow for continuous monitoring of flow rate. The driving force for flow is typically provided by a reservoir raised by some height above the balance but can also be generate by a pressurized water source (tank) or vacuum pump.

Ranges of values edit

Ks: xx-xxx[1]

KL: xx-xxx

ks: xx-xxx

kL: xxx-xxx


Safety considerations edit

Care in handling pressurized gas and acidic flow solutions.

Hazardous materials and disposal edit

Pressurized gas (MSDS sheet)

Titan Review edit

Protocols edit

Pipette method edit

Gold leaf PROTOCOLS

other protocols

Balance method edit

Gold leaf PROTOCOLS

other protocols

Flow meter method edit

Gold leaf PROTOCOLS

other protocols

Other edit

Resources edit

Data analysis edit

Scientific publications edit

  1. ^ Santiago et al Functional Ecology 18: 38-43

Links edit

Related techniques edit

[Leaf hydraulic conductance]

Hydraulic vulnerability

Leaf water potential