Scenarios of phosphorus flow from agriculture and domestic wastewater in Myanmar (2010–2100)

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Abstract

Transfer of nutrients from agriculture and wastewater to the hydrosphere attracts attention of policymakers and scientists due to an increasingly important influence on the water environment. Crop and livestock production and fisheries predominantly support the Myanmar economy. However, phosphorus (P), which is used in cultivation and is also present in domestic sewage, is a major source of biogenic pollutants and eutrophication in Myanmar. It is therefore necessary to elucidate P flows from agricultural and domestic wastewaters to formulate a series of cost-effective policies and best-management practices (BMPs). This paper describes P flows to the hydrosphere, as driven by agricultural and domestic wastewater use in Myanmar during 2010–2100. The results reveal that total P flow from farmland and livestock occurred at 55 thousand Mg/year (thousand million grams per annum) in 2010 but is expected to be 128–141 thousand Mg/year in 2100. Urban population growth is the main factor contributing to the gradual increase in P flow from domestic wastewater; however, most of the P flow is derived from agriculture, suggesting that marked reductions in fertilizer use are necessary. This research provides basic information for the appraisal of P utilization and facilitates the identification of important objectives for sustainable P management in Myanmar.

Figures

  • Table 1. Land use, population, GDP (Gross Domestic Product), crop and livestock production in Myanmar.
  • Figure 1. Simplified flows of P (phosphorus) from agriculture and human sewage to hydrosphere.
  • Table 2. Classification of crops.
  • Table 3. Amount of phosphorus fertilizer (P2O5) per unit of harvested area (Mg/ha).
  • Table 4. Average phosphorus removal ratio (PR) setting based on per-capita GDP PPP (gross domestic product at purchasing power parity)
  • Figure 4. Annual P flow from domestic wastewater to the hydrosphere. Note: PFe1 (high): P flow from blackwater which is discharged by human beings via STFs (sewage treatment facilities) under assumption of high sewage pipeline diffusion ratio; PFe1 (low): P flow from blackwater which is discharged by human beings via STFs (sewage treatment facilities) under assumption of low sewage pipeline diffusion ratio; PFe2 (high): P flow from blackwater which is directly discharged by human beings under assumption of high sewage pipeline diffusion ratio; PFe2 (low): P flow from blackwater which is directly discharged by human beings under assumption of low sewage pipeline diffusion ratio; PFg1 (high): P flow from gray water which is discharged by human beings via STFs and wastewater treatment facilities under assumption of high sewage pipeline diffusion ratio; PFg1 (low): P flow from gray water which is discharged by human beings via STFs and wastewater treatment facilities under assumption of low sewage pipeline diffusion ratio; PFg2 (high): P flow from gray water which is directly discharged by human beings under assumption of high sewage pipeline diffusion ratio; PFg2 (low): P flow from gray water which is directly discharged by human beings under assumption of high sewage pipelin diffu ion ratio.
  • Table 5. Details of six scenarios estimating P flow from agricultural and domestic wastewater (2010–2100).

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CITATION STYLE

APA

Lwin, C. M., Maung, K. N., Murakami, M., & Hashimoto, S. (2017). Scenarios of phosphorus flow from agriculture and domestic wastewater in Myanmar (2010–2100). Sustainability (Switzerland), 9(8). https://doi.org/10.3390/su9081377

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