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Published online 25 May 2007
Published in J Environ Qual 36:963-974 (2007)
DOI: 10.2134/jeq2006.0318
© 2007 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Riparian Plant Material Inputs to the Murray River, Australia

Composition, Reactivity, and Role of Nutrients

Graeme Esslemonta,b, William Mahera,b,*, Phillip Forda,c and Ian Lawrencea

a Cooperative Research Centre for Freshwater Ecology, Univ. of Canberra, ACT 2601 Australia
b Ecochemistry Lab., Institute of Applied Ecology, Univ. of Canberra, ACT 2601 Australia
c CSIRO, Land and Water. GPO Box 1666, Canberra, ACT, 2601


Figure 1
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Fig. 1. Sampling sites along the Murray and Murrumbidgee rivers.

 

Figure 2
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Fig. 2. Proximate organic components (% mass) in fresh material (dark shading), abscission material (light shading), and weathered material. Data are means ±2 standard errors.

 

Figure 3
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Fig. 3. Principal components of riparian plant materials based on molecular proximate components, plus total carbon, nitrogen, and phosphorus. Codes for plant materials are given in Table 1. Zla represents the superposition of plant materials Ala, Bla, and Cla. Classification of plant materials (flexible unweighted pair-group method using arithmetic averages [UPGMA], ß = –0.1) shows the grouping of leaf litter compositions. Visually recognizable plant material circled in the ordination ([1] Eucalyptus leaf; [2] Eucalyptus bark and C. cunninghamiana seed cone; [3] Grasses; [4] Macrophytes; [5] Aquatic herbs; [6] Non-eucalypt leaves), are symbolized in the classification. TN, total nitrogen; TP, total phosphorus.

 

Figure 4
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Fig. 4. (a–f) Isotopic ratios of {delta}13C and {delta}15N in riparian plant materials.

 

Figure 5
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Fig. 5. Aerobic mineralization of plant materials, represented as cumulative biological oxygen demand (BOD) (M O2 consumed per M C in the original biomass) over time (d). Average measurement errors (standard error) were 0.005 to 0.015 mole/mole O2.C–1 for most plant materials, 0.025 mole/mole O2.C–1 for Typha sp., and 0.033 mole/mole O2.C–1 for Lolium sp.

 

Figure 6
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Fig. 6. Aerobic mineralization of plant material: (a, d) Rate constants (k1 and k2), fractions of (b) reactive carbon (C1) and (e) refractory carbon (C2), and the reactive product (C.k) that represents the biodegradable carbon fractions during the (c) first and (f) second decay stages of decay.

 

Figure 7
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Fig. 7. (a–d) Ratios of C/N relative to {delta}13C in plant materials.

 

Figure 8
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Fig. 8. (a, b) Total N and P in plant material. Means ± maximum and minimum values.

 





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The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
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Vadose Zone Journal
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