Dynamic modeling of the growth of Phragmites australis: model description

By T. Asaeda, S. Karunaratne. 2000

147 citations recorded by the source corpus.

Subfields: Earth-Surface Processes, Ecology, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/112f3ba91e150d771c22d886a8d06587957be646

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Earth-Surface Processes

1. N. Sahara
2. J. Manatunge
3. Lalith Rajapakse
4. T. Asaeda

In Ecology

1. Jack J. Middelburg
2. Karline Soetaert
3. D. Oevelen
4. N. Sahara
5. J. Manatunge
6. Lalith Rajapakse
7. Patrick Meire
8. Maurice Hoffmann

In Global and Planetary Change

1. Jack J. Middelburg
2. N. Sahara
3. J. Manatunge
4. Lalith Rajapakse
5. Maurice Hoffmann
6. T. Asaeda
7. Karline Soetaert

Citations in the corpus

• Modeling growth and carbon allocation in two reed beds (Phragmites australis) in the Scheldt estuary (2004, methodology): “It merges process descriptions from the reed model of (Asaeda and Karunaratne, 2000; hereafter denoted as AK2000) and the crop model Simple and Universal CROp Simulation (SUCROS; Penning de Vries and Van Laar, 1982; Goudriaan and Van Laar, 1994).”
• The Effect of Summer Harvesting of Phragmites australis on Growth Characteristics and Rhizome Resource Storage (2005, methodology): “Previous studies (Husak, 1978; Bjorndahl, 1985; Gryseels, 1989a, b; Asaeda & Karunaratne, 2000; Asaeda et al., 2002, 2003) have suggested the best season to cut, but they are conflicting.”
• Biogenic silica in tidal freshwater marsh sediments and vegetation (Schelde estuary, Belgium) (2005, background): “Low BSi contents in roots were reflected in only 5 to 10 t of BSi stored in non-rhizomeous roots in the upper 30 cm. BSi in P. australis rhizomes would account for about 10 to 20 t of BSi, if we estimate rhizome biomass production at 2500 g m–2 (Schierup 1978, Asaeda & Karunaratne 2000).”