Abstract:The water hyacinth (Eichhornia crassipes (Mart.) Solms.) plants in lakes and reservoirs have gained considerable attention in tropical and sub-tropical parts of the world due to its rapid growth. The amount of nutrients released from the dead plant materials is of particular interest. Thus, decomposition of water hyacinth plant parts under aerobic conditions was studied in the laboratory. Roots, petioles, and leaves of water hyacinth were enclosed separately in one litre polypropylene bottles which contained 5… Show more
“…9, 2016 was minimal during this period. 11,23 The mass loss during this time is associated with the release of cytoplasmic fractions and hydrosoluble compounds that were present in the macrophyte. 24,25 The release of phosphorus during the initial decomposition period is linked to the loss of soluble phosphorus that had accumulated in plant tissue vacuoles.…”
Section: Discussionmentioning
confidence: 99%
“…At the end of 90 days, 234 mg of chloramphenicol was added to each chamber containing samples treated with antibiotics to suppress bacterial growth. 11,14 The decomposition experiment was conducted for 120 days, and samples from each treatment were randomly collected at eight sampling times: 1, 3, 7, 15, 30, 60, 90 and 120 days.…”
Section: Methodsmentioning
confidence: 99%
“…The detritus decomposition was exponentially modeled as proposed by Gamage and Asaeda: 11 W t = W 0 e −kt (1) where W t is the dry weight at time t, W 0 is the initial dry weight and k is the decay rate constant. By using this model, we assumed that the decomposition process follows firstorder kinetics and that the decomposition rate constant at time t is proportional to the weight at time t. The decay rate was calculated using the equation 1.…”
Section: Methodsmentioning
confidence: 99%
“…[11][12][13] The main changes in nutrient forms occur during the catabolism stage of the decomposition process, with formation of phenolic compounds, humic substances, and phosphorous derivatives. Microorganisms incorporate inorganic nutrients from senescent biomass and exert an overall impact on both the internal wetland nutrient dynamics and overall nutrient sequestration, both of which are important functions of wetlands in the landscape.…”
The study of the Typha species has gained attention in tropical areas due to their rapid growth, nutrient release, and contribution to detritus in lakes. Analysis of the degradation of Typha angustifolia has shown that the first stage of decomposition is marked primarily by the release of soluble compounds, indicating that microorganisms have a minor influence at this stage. In subsequent stages, microorganisms act by degrading and consuming phenolic compounds and phosphorus. The remaining compounds form humic substances and are retained in the detritus. Thus, microorganisms significantly degrade organic matter, resulting in a two-fold increase in decomposition. Different forms of phosphorus could be detected in the remaining mass by 31 P NMR (nuclear magnetic resonance). By comparing the 31 P NMR data between the samples with and without the antibiotic, we can better understand the slow decomposition process of Typha angustifolia.
“…9, 2016 was minimal during this period. 11,23 The mass loss during this time is associated with the release of cytoplasmic fractions and hydrosoluble compounds that were present in the macrophyte. 24,25 The release of phosphorus during the initial decomposition period is linked to the loss of soluble phosphorus that had accumulated in plant tissue vacuoles.…”
Section: Discussionmentioning
confidence: 99%
“…At the end of 90 days, 234 mg of chloramphenicol was added to each chamber containing samples treated with antibiotics to suppress bacterial growth. 11,14 The decomposition experiment was conducted for 120 days, and samples from each treatment were randomly collected at eight sampling times: 1, 3, 7, 15, 30, 60, 90 and 120 days.…”
Section: Methodsmentioning
confidence: 99%
“…The detritus decomposition was exponentially modeled as proposed by Gamage and Asaeda: 11 W t = W 0 e −kt (1) where W t is the dry weight at time t, W 0 is the initial dry weight and k is the decay rate constant. By using this model, we assumed that the decomposition process follows firstorder kinetics and that the decomposition rate constant at time t is proportional to the weight at time t. The decay rate was calculated using the equation 1.…”
Section: Methodsmentioning
confidence: 99%
“…[11][12][13] The main changes in nutrient forms occur during the catabolism stage of the decomposition process, with formation of phenolic compounds, humic substances, and phosphorous derivatives. Microorganisms incorporate inorganic nutrients from senescent biomass and exert an overall impact on both the internal wetland nutrient dynamics and overall nutrient sequestration, both of which are important functions of wetlands in the landscape.…”
The study of the Typha species has gained attention in tropical areas due to their rapid growth, nutrient release, and contribution to detritus in lakes. Analysis of the degradation of Typha angustifolia has shown that the first stage of decomposition is marked primarily by the release of soluble compounds, indicating that microorganisms have a minor influence at this stage. In subsequent stages, microorganisms act by degrading and consuming phenolic compounds and phosphorus. The remaining compounds form humic substances and are retained in the detritus. Thus, microorganisms significantly degrade organic matter, resulting in a two-fold increase in decomposition. Different forms of phosphorus could be detected in the remaining mass by 31 P NMR (nuclear magnetic resonance). By comparing the 31 P NMR data between the samples with and without the antibiotic, we can better understand the slow decomposition process of Typha angustifolia.
“…Much research has been devoted to the decomposition of water hyacinth [3,5,8,11,12,13,15,17,18,25,26,41]. Studies have shown that bacterial decay activity occurs most rapidly within the first 14 days of decomposition [8,11,13,25,41].…”
Here we explore the utilization of Eichhornia crassipes, commonly known as water hyacinth, as a competitive source of biomass for conversion to fuel. Ecologically, E. crassipes is the most undesirable of a class of noxious and invasive aquatic vegetation. Water hyacinth grows rapidly on the surface of waterways, forming a dense mat which depletes the surrounding environment of essential nutrients. These properties, rarely encountered in other plant systems, are features of an ideal feedstock for renewable biomass. The high characteristic water content limits the range over which the material can be transported; however it also makes E. crassipes a natural substrate for rapid microbial metabolism that can be employed as a potentially effective biological pretreatment technology. We show through a life cycle analysis that water hyacinth is a competitive feedstock with the potential to be produced at a cost of approximately 40 dollars per ton of dry mass.
Tropical wetlands are not included in Earth system models, despite being an important source of methane (CH4) and contributing a large fraction of carbon dioxide (CO2) emissions from land use, land use change, and forestry in the tropics. This review identifies a remarkable lack of data on the carbon balance and gas fluxes from undisturbed tropical wetlands, which limits the ability of global change models to make accurate predictions about future climate. We show that the available data on in situ carbon gas fluxes in undisturbed forested tropical wetlands indicate marked spatial and temporal variability in CO2 and CH4 emissions, with exceptionally large fluxes in Southeast Asia and the Neotropics. By upscaling short-term measurements, we calculate that approximately 90 ± 77 Tg CH4 year−1 and 4540 ± 1480 Tg CO2 year−1 are released from tropical wetlands globally. CH4 fluxes are greater from mineral than organic soils, whereas CO2 fluxes do not differ between soil types. The high CO2 and CH4 emissions are mirrored by high rates of net primary productivity and litter decay. Net ecosystem productivity was estimated to be greater in peat-forming wetlands than on mineral soils, but the available data are insufficient to construct reliable carbon balances or estimate gas fluxes at regional scales. We conclude that there is an urgent need for systematic data on carbon dynamics in tropical wetlands to provide a robust understanding of how they differ from well-studied northern wetlands and allow incorporation of tropical wetlands into global climate change models.
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