Filtering by
- All Subjects: Food Systems
- All Subjects: Water
- All Subjects: Nitrogen
- Creators: School of Sustainability
In 2021, Palestine will have been under official Israeli occupation for 54 years. As conflict persists between the two populations, it is becoming increasingly difficult to imagine a peaceful resolution. As international legal bodies have failed to bring an end to the occupation, the Israeli government continues to carry out extensive violations of human rights against the Palestinians. One significant consequence of the occupation has been the Palestinians’ lack of access to safe and reliable water, a problem that is continuing to worsen as a result of climate change and years of over-utilization of shared, regional water resources. Since the occupation started, international organizations have not only affirmed the general human right to water but have overseen several peace agreements between Israel and Palestine that have included stipulations on water. Despite these measures, neither water access nor quality has improved and, over time, has worsened. This paper will look at why international law has failed to improve conditions for Palestinians and will outline the implications of the water crisis on a potential solution between Israel and Palestine.
The rise in urban populations is encouraging cities to pursue sustainable water treatment services implementing constructed treatment wetlands (CTW). This is especially important in arid climates where water resources are scarce; however, research regarding aridland CTWs is limited. The Tres Rios CTW in Phoenix, Arizona, USA, presents the tradeoff between greater water loss and enhanced nitrogen (N) removal. Previous research has suggested that water loss due to transpiration is replaced by a phenomenon termed the Biological Tide. This trend has been documented since 2011 by combining transpiration values with a nitrogen budget. Calculations were made at both the marsh and whole-system scale. The purpose of this paper is to demonstrate how the Biological Tide enhances N uptake throughout the CTW. Results indicate that about half of the nitrogen taken up by the vegetated marsh is associated with new water entering the marsh via the Biological Tide with even higher values during warmer months. Furthermore, it is this phenomenon that enhances N uptake throughout the year, on average, by 25.9% for nitrite, 9.54% for nitrate, and 4.84% for ammonium at the whole-system scale and 95.5%, 147%, and 118% within the marsh. This paper demonstrates the Biological Tide’s significant impact on enhanced N removal in an aridland CTW.