The Law of Transboundary Aquifers: Many Ways of Going Forward, but Only One Way of Standing Still

Published date01 April 2014
DOIhttp://doi.org/10.1111/reel.12067
AuthorFrancesco Sindico,Gabriel Eckstein
Date01 April 2014
The Law of Transboundary Aquifers: Many Ways of
Going Forward, but Only One Way of Standing Still
Gabriel Eckstein and Francesco Sindico
The international community has been considering
international legal norms and policies for the manage-
ment of transboundary aquifers for more than ten
years. In 2008, the International Law Commission
provided a framework with the adoption of the Draft
Articles on the Law of Transboundary Aquifers, which
are now formally annexed to a United Nations General
Assembly (UNGA) Resolution. Since 2008, the topic of
the law of transboundary aquifers has thrice been
placed on the agenda of the UNGA Sixth Committee
with a specific mandate to discuss the future form of
the Draft Articles. This article explores the options
before the international community regarding the
future form of the Draft Articles and considers the
possible advantages and disadvantages of each
option. The article also discusses the extent to which
the actual form of the Draft Articles matters in itself, or
whether their impact ultimately will depend on other
factors.
INTRODUCTION
Groundwater resources play a critical role in providing
fresh water for people, industries, nations and the envi-
ronment worldwide. Globally, groundwater provides
approximately 45% of humanity’s freshwater needs for
everyday domestic uses, such as drinking, cooking and
hygiene, as well as 24% of water used in irrigated agri-
culture.1In many cases, groundwater is found in aqui-
fers that are transboundary.2While 276 international
watercourses traverse the world’s land areas,3an
ongoing study has identified, to date, 448 aquifers and
aquifer bodies traversing international political bound-
aries.4In places like the Middle East, North Africa and
the Mexico-United States border, transboundary aqui-
fers serve as the primary or sole source of available
freshwater for human and environmental sustenance.
Recognizing the particular importance of trans-
boundary aquifers, nations and international agencies
around the world have begun exploring mechanisms for
governing these hidden resources. This includes formal
efforts to manage and regulate transboundary aquifers,
such as the rigorous scheme implemented on the Gene-
vese Aquifer along the French-Swiss border,5to more
general cooperative regimes, such as the Guarani
Aquifer Agreement in South America,6to instruments
aimed mainly at an initial exchange of scientific data, as
developed for the Nubian Sandstone and North Western
Sahara aquifer systems in Northern Africa.7It also
includes informal efforts forged by subnational political
entities, like the unofficial arrangements crafted for the
Hueco Bolson aquifer underlying the cities of Juárez and
El Paso on the Mexico-United States border,8and for the
1J. Margat and J. van der Gun, Groundwater around the World: A
Geographic Synopsis (CRC Press, 2013), at 149.
2It is important to highlight that groundwater is just one component of
an aquifer; an aquifer is the geological formation that contains the
groundwater. According to the International Law Commission Draft
Articles on the Law of Transboundary Aquifers, an aquifer is ‘a per-
meable water bearing geological formation underlain by a less per-
meable layer and the water contained in the saturated zone of the
formation’. The Law of Transboundary Aquifers (UNGA Resolution
A/RES/63/124, 11 December 2008), Article 2a.
3P. Wouters and R. Moynihan, ‘Benef‌it Sharing in the UN Water-
courses Convention and under International Water Law’, in: F.
Rocha Loures and A. Rieu-Clarke (eds.), The UN Watercourses
Convention in Force: Strengthening International Law for
Transboundary Water Management (Routledge, 2013), 336.
4See International Groundwater Assessment Centre (IGRAC),
‘Transboundary Aquifers of the World: Update 2012, Special Edition
for the 6th World Water Forum, Marseille’, found at: <http://www.un-
igrac.org/dynamics/modules/SFIL0100/view.php?f‌il_Id=213>.
5Convention Relative a la Protection, a l’Utilisation, a la
Realimentation et au Suivi de la Nappe Souterraine Franco-Suisse du
Genevois (18 December 2007; in force 1 January 2008).
6Acuerdo Sobre el Acuífero Guarani (San Juan, Argentina, 2 August
2010; not yet in force), (‘Guarani Aquifer Agreement’). An
English version of the Agreement can be found at: <http://www
.internationalwaterlaw.org/documents/regionaldocs/Guarani_Aquifer
_Agreement-English.pdf>.
7The Nubian Sandstone Aquifer System underlies the territories of
Chad, Egypt, Libya and Sudan. See Programme for the Development
of a Regional Strategy for the Utilisation of the Nubian Sandstone
Aquifer System (NSAS): Terms of Reference for the Monitoring and
Exchange of Groundwater Information of the Nubian Sandstone
Aquifer System (Tripoli, 5 October 2000), found at: <http://www.fao
.org/docrep/008/y5739e/y5739e05.htm>. The North Western Sahara
Aquifer System underlies Algeria, Libya and Tunisia. See Establish-
ment of a Consultation Mechanism for the Northwestern Sahara
Aquifer System (SASS) (Rome, 19–20 December; endorsed 6
January 2003 (Algeria), 15 February 2003 (Tunisia), 23 February
2003 (Libya)), found at: <http://www.fao.org/docrep/008/y5739e/
y5739e05.htm#bm05.2.1>.
8Memorandum of Understanding between City of Juárez, Mexico
Utilities and the El Paso Water Utilities Public Services Board of the
City of El Paso, Texas (6 December 1999), found at: <http://
internationalwaterlaw.org/documents/regionaldocs/Local-GW-
Agreements/El_Paso-Juarez_MoU.pdf>.
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Review of European Community & International Environmental Law
RECIEL 23 (1) 2014. ISSN 2050-0386 DOI: 10.1111/reel.12067
© 2014 John Wiley & Sons Ltd, 9600 Garsington Road, Oxford OX4 2DQ, UK and 350 Main Street, Malden, MA 02148, USA.
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