Seminar Report on Transboundary Aquifers and International Law: The Experience of the Guarani Aquifer System, University of Surrey, Guildford, UK, 31 August 2010

2010 ◽  
Vol 26 (4) ◽  
pp. 715-718
Author(s):  
Francesco Sindico
2011 ◽  
Vol 13 (3) ◽  
pp. 255-272 ◽  
Author(s):  
Francesco Sindico

AbstractArgentina, Brazil, Paraguay and Uruguay signed the Guarani Aquifer Agreement on 2 August 2010. This is the first international treaty regarding the management of a specific transboundary aquifer to have been adopted after the UN International Law Commission (UNILC) adopted the Draft Articles on the Law of Transboundary Aquifers, which have been annexed to UN General Assembly Resolution 63/124. The latter encourages States to take into account the Draft Articles when devising arrangements for the management of specific transboundary aquifers. The Guarani Aquifer Agreement, therefore, is a first response to this call from the international community. In this article the background to the Guarani Aquifer Agreement is explored, including an overview of the key characteristics of the Guarani Aquifer System and the steps that have led to the adoption of the Guarani Aquifer Agreement. Sovereignty, the obligation to cooperate and the incipient institutional framework are discussed as key elements arising from the Guarani Aquifer Agreement. Finally, the article argues that a link between the latter and the UNILC Draft Articles can be appreciated. This link has important practical implications especially in relation to the applicability of the UNILC Draft Articles for interpretation purposes of the Guarani Aquifer Agreement.


AJIL Unbound ◽  
2021 ◽  
Vol 115 ◽  
pp. 178-182
Author(s):  
Francesco Sindico

Could Turkey dam the Tigris and Euphrates and deprive its downstream neighbors of vital water resources? Could Brazil over-pump the Guarani Aquifer System to the detriment of the other aquifer states? Could Egypt put pressure on upstream Nile states and prevent them from developing river related infrastructure that might limit downstream flow? International law in the field of transboundary water cooperation has evolved and would appear to condemn unilateral practices such as the ones suggested above. However, hydro politics and the lack of reception of international water law instruments by many countries sometimes make it difficult to see international law properly reflected in the management of major rivers, lakes and aquifers around the world. In this essay, I first highlight what international law dictates when it comes to the tension between national sovereignty and transboundary water cooperation. I then explore how this tension plays out in the three examples noted above. Due to limited acceptance of the existing international, bilateral, or regional legal instruments, the resolution of the tension between national sovereignty and transboundary water cooperation will often be left to customary international law.


2011 ◽  
Vol 13 (3) ◽  
pp. 291-304
Author(s):  
Felix Zaharia

AbstractAt the beginning of April 2011, local water companies from the counties of Arad in Romania and Békés in Hungary initiated the demarches for the first project of transboundary supply of groundwater from the Romanian part of the Mureş Alluvial Fan Aquifer System to consumers in Hungary. An idea which came about at the same time that the International Law Commission’s Draft Articles on the Law of Transboundary Aquifers were being adopted, will be probably put into practice shortly after the United Nations General Assembly would have analyzed whether to transform the Draft Articles into a multilateral treaty. Until then, many legal questions regarding this project must be answered, some of them national, others international. This article tries to answer some of these problems, with the help of the International Law Commission’s Draft Articles on the Law of Transboundary Aquifers and the bilateral agreements concluded between Romania and Hungary.


2016 ◽  
Vol 15 (2) ◽  
pp. 249-263
Author(s):  
Catherine Tinker

The Guarani Aquifer Accord of 2010 represents a plan for the multiple, sustainable, equitable and reasonable use of the water of the Guarani Aquifer System and a pledge to prevent significant harm to this vast natural resource in South America. Based on good science and good international law, this regional agreement was reached by Brazil, Argentina, Uruguay and Paraguay, acknowledging the environmental, economic and geopolitical importance of the underground water linking the four states known as the “Guarani Aquifer System.” The Guarani Aquifer Accord (“Acordo sobre o Aquífero Guarani” or “Acuerdo Aquífero Guarani”) is the first regional treaty to be modeled after the International Law Commission Draft Articles on Transboundary Aquifers of 2008, which address “confined” aquifers that are outside the scope of the United Nations Watercourses Convention of 1997. This article explores the Guarani Aquifer Accord’s provisions for exchanges of scientific and technical information, notification and consultation, direct negotiations, referral to a joint commission to be created once the Accord enters into force for evaluation and recommendations in case of a dispute, and the option of a subsequent arbitration protocol to be negotiated in future. Taken together, procedural requirements and the provisions in the Accord in favor of diplomatic and political resolution of future disputes over the use and protection of the water may forestall the need to resort to litigation in international courts or tribunals. This article concludes that, even absent an additional protocol for arbitration of disputes and absent the establishment of a joint commission to facilitate information exchange, convene regular meetings and build trust as contained in the agreement, the Guarani Aquifer Accord provides a framework for regional cooperation designed to avoid or resolve conflicts.


2012 ◽  
Vol 106 (2) ◽  
pp. 322-340 ◽  
Author(s):  
Donald McRae

On November 17, 2011, the UN General Assembly elected the members of the International Law Commission for the next five years. In the course of the quinquennium that was completed in August 2011 with the end of the sixty-third session, the Commission concluded four major topics on its agenda: the law of transboundary aquifers, the responsibility of international organizations, the effect of armed conflicts on treaties, and reservations to treaties. It was by any standard a substantial output. The beginning of a new quinquennium now provides an opportunity to assess what the Commission has achieved, to consider the way it operates, and to reflect on what lies ahead for it.


2008 ◽  
Vol 35 (2) ◽  
pp. 115 ◽  
Author(s):  
ANA PAULA SOARES ◽  
PAULO CÉSAR SOARES ◽  
MICHAEL HOLZ

The stratigraphic register of the Guarani aquifer system in the Parana basin involves deposits of the Triassic to the Cretaceous. The register in the south region differs from the other areas of the basin, causing confusion in the stratigraphic conception of the Pirambóia Formation. This formation is correlated with paleozoics deposits whose register is only found in the south region of the basin. The correlation that intends for these units has implications in the space configuration and distribution of the aquifer. The space relationships of this record are reinterpreted. The Rio do Rasto Formation, of late Permian age record alluvial plain system, in a progressive semiarid environment, including dune fields; in the southern part of the basin these dune field are extensive and is represented by thick record, covered again by extensive fluvial deposits of the Sanga do Cabral Fm at the PT boundary. The unconformity above records a generalized uplift, associated to the Gondwanides orogeny and to climatic changes, accompanied by progressive supply and sin-sedimentary deformation. Above the unconformity, aeolian and fluvial deposits of the Mesozoic sequence present division organized in 3 blocks: West, Central and East. Three depositional cycles were identified. The first, unconformable over Permian rocks, occurs only in the Central Block, with fluvial and lacustrine deposits filling small rifts (Santa Maria and Caturrita fms). The second cycle extends over the whole basin with fluvial deposits and humid aeolian (formations Guará and Pirambóia); the fluvial and aeolian Guará Fm lies unconformable over Sanga do Cabral Fm in the West Block. In the East Block the aeolian and fluvial unit identified as Pirambóia Fm correlative; it occurs unconformable over the Rio do Rasto Fm, omitting the Sanga do Cabral Fm and the rocks of the first cycle. The third cycle system tract records super arid dune fields of the Botucatu Formation. The Late Permian aeolian facies of the Sanga do Cabral Fm, previously called by some authors as the Pirambóia Fm, doesn't present interfingers and doesn't constitute a hydrostratigraphic unit connected to the Guarani System.


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