Effects of litter and fine root composition on their decomposition in a Rhodic Paleustalf under different land uses

Plant litter and fine roots are important in maintaining soil organic carbon (C) levels as well as for nutrient cycling. The decomposition of surface-placed litter and fine roots of wheat ( Triticum aestivum ), lucerne ( Medicago sativa ), buffel grass ( Cenchrus ciliaris ), and mulga ( Acacia aneura ), placed at 10-cm and 30-cm depths, was studied in the field in a Rhodic Paleustalf. After 2 years, = 60% of mulga roots and twigs remained undecomposed. The rate of decomposition varied from 4.2 year -1 for wheat roots to 0.22 year -1 for mulga twigs, which was significantly correlated with the lignin concentration of both tops and roots. Aryl+O-aryl C concentration, as measured by 13 C nuclear magnetic resonance spectroscopy, was also significantly correlated with the decomposition parameters, although with a lower R 2 value than the lignin concentration. Thus, lignin concentration provides a good predictor of litter and fine root decomposition in the field.

Upper level, C House, Coorparoo, Brisbane

View along North-West elevation upper level.

Iwan, C House, Coorparoo, Brisbane

As seen from pool deck.

The Nest, C House, Coorparoo, Brisbane

Timber deck with built-in seat overlooking greater landscape beyond.

Pool deck, C House, Coorparoo, Brisbane

View back towards house from deck. with Iwan (right) and filter room (left).

The Nest, C House, Coorparoo, Brisbane

Concrete framework for The Nest (North-West elevation), with timber framework yet to be added.

North-West elevation, C House, Cooparoo, Brisbane

Entry stair in foreground.

Pool deck, C House, Coorparoo, Brisbane

As seen from The Nest above

Outdoor room, C House, Coorparoo, Brisbane

As seen from upper level of house.

Lower level interior, C House, Coorparoo, Brisbane

View to landcape beyond from lower level interior.