Delineation of water flow paths in a tropical Andean headwater catchment with deep soils and permeable bedrock-Reference-Cited by-同舟云学术

Delineation of water flow paths in a tropical Andean headwater catchment with deep soils and permeable bedrock

Published:2022-10 Issue:10 Volume:36 Page:
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Lahuatte Braulio¹²,Mosquera Giovanny M.³^ORCID,Páez‐Bimos Sebastián⁴⁵^ORCID,Calispa Marlon⁶⁷,Vanacker Veerle⁴,Zapata‐Ríos Xavier⁵,Muñoz Teresa⁸,Crespo Patricio²^ORCID

Affiliation:

1. Fondo para la Protección del Agua de Quito–FONAG, Av. Mariana de Jesús Quito Ecuador

2. Departamento de Recursos Hídricos y Ciencias Ambientales Facultad de Ingeniería & Facultad de Ciencias Químicas, Universidad de Cuenca Cuenca Ecuador

3. Instituto Biósfera, Universidad San Francisco de Quito USFQ, Diego de Robles y Vía Interoceánica Quito Ecuador

4. George Lemaître Center for Earth and Climate Research Earth and Life Institute, UCLouvain Louvain‐la‐Neuve Belgium

5. Departamento de Ingeniería Civil y Ambiental, Facultad de Ingeniería Civil y Ambiental Escuela Politécnica Nacional Quito Ecuador

6. Earth and Life Institute, Environmental Sciences Université catholique de Louvain Louvain‐la‐Neuve Belgium

7. Programa para el Manejo de Agua y Suelo (PROMAS), Facultad de Ingeniería Civil Universidad de Cuenca Cuenca Ecuador

8. Empresa Pública Metropolitana de Agua Potable y Saneamiento (EPMAPS) Quito Ecuador

Publisher

Wiley

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.14725

Reference84 articles.

1. Ecohydrological drivers of Neotropical vegetation in montane ecosystems

2. Flow path depth is the main controller of mean base flow transit times in a mountainous catchment

3. Residence times and flow paths of water in steep unchannelled catchments, Tanakami, Japan

4. Importance of Fog and Cloud Water Contributions to Soil Moisture in the Andean Páramo

5. Willamette River Basin surface water isoscape (δ18O and δ2H): temporal changes of source water within the river

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