The Tribal Sovereign as Citizen: Protecting Indian Country Health and Welfare Through Federal Environmental Citizen Suits

This Article suggests that federal environmental citizen suits can serve tribal sovereignty interests without presenting the legal risks tribes face when they attempt direct regulation of non-Indians. Section I briefly describes governmental regulatory roles tribes may play in the implementation of federal environmental law and policy. Section II overviews the conceptual and procedural framework for tribal claims as citizens. Section III argues that in bringing environmental citizen suits, tribal governments exercise their inherent sovereign power and responsibility to protect the health and welfare of tribal citizens and the quality of the Indian country environment. Section IV concludes that, while suits directed at one facility cannot and should not replace comprehensive tribal programs, they offer concrete benefits to tribes without risking adverse judicial decisions on the scope of tribal sovereignty and Indian country

Las relaciones bilaterales Ecuador-Colombia: acuerdos bilaterales vigentes y su aplicación

La Policía Nacional, a través del Servicio de Migración, tiene la obligación legal de controlar, tanto la salida como la entrada de extranjeros, de territorio ecuatoriano, en cumplimiento a las disposiciones de la Ley de Migración y su Reglamento, y especialmente con relación a los ciudadanos colombianos que ingresan a nuestro país, gozando de un tratamiento especial, por efecto de los acuerdos binacionales suscritos y vigentes entre Ecuador y Colombia. La Policía Nacional, por carecer de los suficientes recursos humanos y materiales, pese a su buena voluntad, no puede cumplir con su misión; en tal virtud, recibe la asistencia de parte de las Fuerzas Armadas ecuatorianas, y especialmente del Ejército, que presta su contingente, especialmente en el sitio fronterizo de La Punta. El Jefe Militar del Destacamento de La Punta (General Farfán), informa periódicamente a la Jefatura de Migración de Sucumbíos, mediante los listados correspondientes, el movimiento migratorio de los ciudadanos colombianos, quienes por pasar por el referido control, cumplen con todas las formalidades de ley. En vista de la gran extensión del río San Miguel y su cuenca hidrográfica -límite geográfico entre Ecuador y Colombia-, esta situación no permite un adecuado control del movimiento migratorio de nacionales colombianos hacia territorio ecuatoriano y, en consecuencia, sus actividades también serán ilegales o ilícitas, incluyendo acciones de guerrilla, narcotráfico y narco-guerrilla, especialmente

Upper mantle rheology from GRACE and GPS postseismic deformation after the 2004 Sumatra‐Andaman earthquake

International audience[1] Mantle rheology is one of the essential, yet least understood, material properties of our planet, controlling the dynamic processes inside the Earth's mantle and the Earth's response to various forces. With the advent of GRACE satellite gravity, measurements of mass displacements associated with many processes are now available. In the case of mass displacements related to postseismic deformation, these data may provide new constraints on the mantle rheology. We consider the postseismic deformation due to the M w = 9.2 Sumatra 26 December 2004 and M w = 8.7 Nias 28 March 2005 earthquakes. Applying wavelet analyses to enhance those local signals in the GRACE time varying geoids up to September 2007, we detect a clear postseismic gravity signal. We supplement these gravity variations with GPS measurements of postseismic crustal displacements to constrain postseismic relaxation processes throughout the upper mantle. The observed GPS displacements and gravity variations are well explained by a model of visco-elastic relaxation plus a small amount of afterslip at the downdip extension of the coseismically ruptured fault planes. Our model uses a 60 km thick elastic layer above a viscoelastic asthenosphere with Burgers body rheology. The mantle below depth 220 km has a Maxwell rheology. Assuming a low transient viscosity in the 60–220 km depth range, the GRACE data are best explained by a constant steady state viscosity throughout the ductile portion of the upper mantle (e.g., 60–660 km). This suggests that the localization of relatively low viscosity in the asthenosphere is chiefly in the transient viscosity rather than the steady state viscosity. We find a 8.10 18 Pa s mantle viscosity in the 220–660 km depth range. This may indicate a transient response of the upper mantle to the high amount of stress released by the earthquakes. To fit the remaining misfit to the GRACE data, larger at the smaller spatial scales, cumulative afterslip of about 75 cm at depth should be added over the period spanned by the GRACE models. It produces only small crustal displacements. Our results confirm that satellite gravity data are an essential complement to ground geodetic and geophysical networks in order to understand the seismic cycle and the Earth's inner structure

Admission profile and discharge outcomes for infants aged less than 6 months admitted to inpatient therapeutic care in 10 countries: a secondary data analysis

Evidence on the management of acute malnutrition in infants aged less than 6 months (infants <6mo) is scarce. To understand outcomes using current protocols, we analysed a sample of 24,045 children aged 0-60 months from 21 datasets of inpatient therapeutic care programmes in 10 countries. We compared the proportion of admissions, the anthropometric profile at admission, and the discharge outcomes between infants <6mo and children aged 6-60 months (older children). Infants <6mo accounted for 12% of admissions. The quality of anthropometric data at admission was more problematic in infants <6mo than in older children with a greater proportion of missing data (a 6.9 percentage points difference for length values, 95%CI: 6.0; 7.9, p<0.01), anthropometric measures that could not be converted to indices (a 15.6 percentage points difference for weight-for-length z-score values, 95%CI: 14.3; 16.9, p<0.01), and anthropometric indices that were flagged as outliers (a 2.7 percentage points difference for any anthropometric index being flagged as an outlier, 95%CI: 1.7; 3.8, p<0.01). A high proportion of both infants <6mo and older children were discharged as recovered. Infants <6mo showed a greater risk of death during treatment (risk ratio 1.30, 95%CI: 1.09; 1.56, p<0.01). Infants <6mo represent an important proportion of admissions to therapeutic feeding programmes and there are crucial challenges associated with their care. Systematic compilation and analysis of routine data for infants <6mo is necessary for monitoring programme performance and should be promoted as a tool to monitor the impact of new guidelines on care

Admission profile and discharge outcomes for infants aged less than 6 months admitted to inpatient therapeutic care in 10 countries. A secondary data analysis.

Evidence on the management of acute malnutrition in infants aged less than 6 months (infants &lt;6mo) is scarce. To understand outcomes using current protocols, we analysed a sample of 24 045 children aged 0-60 months from 21 datasets of inpatient therapeutic care programmes in 10 countries. We compared the proportion of admissions, the anthropometric profile at admission and the discharge outcomes between infants &lt;6mo and children aged 6-60 months (older children). Infants &lt;6mo accounted for 12% of admissions. The quality of anthropometric data at admission was more problematic in infants &lt;6mo than in older children with a greater proportion of missing data (a 6.9 percentage point difference for length values, 95% CI: 6.0; 7.9, P &lt; 0.01), anthropometric measures that could not be converted to indices (a 15.6 percentage point difference for weight-for-length z-score values, 95% CI: 14.3; 16.9, P &lt; 0.01) and anthropometric indices that were flagged as outliers (a 2.7 percentage point difference for any anthropometric index being flagged as an outlier, 95% CI: 1.7; 3.8, P &lt; 0.01). A high proportion of both infants &lt;6mo and older children were discharged as recovered. Infants &lt;6mo showed a greater risk of death during treatment (risk ratio 1.30, 95% CI: 1.09; 1.56, P &lt; 0.01). Infants &lt;6mo represent an important proportion of admissions to therapeutic feeding programmes, and there are crucial challenges associated with their care. Systematic compilation and analysis of routine data for infants &lt;6mo is necessary for monitoring programme performance and should be promoted as a tool to monitor the impact of new guidelines on care