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| "notes": "The EDI Data Portal contains environmental and ecological | | "notes": "The EDI Data Portal contains environmental and ecological |
| data packages contributed by a number of participating organizations. | | data packages contributed by a number of participating organizations. |
| Data providers make every effort to release data in a timely fashion | | Data providers make every effort to release data in a timely fashion |
| and with attention to accurate, well-designed and well-documented | | and with attention to accurate, well-designed and well-documented |
| data. To understand data fully, please read the associated metadata | | data. To understand data fully, please read the associated metadata |
| and contact data providers if you have any questions. Data may be used | | and contact data providers if you have any questions. Data may be used |
| in a manner conforming with the license information found in the | | in a manner conforming with the license information found in the |
n | \u201cIntellectual Rights\u201d section of the data package metadata | n | \u201a\u00c4\u00faIntellectual Rights\u201a\u00c4\u00f9 section of the |
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| shall not be liable for any damages resulting from misinterpretation | | Environmental Data Initiative shall not be liable for any damages |
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| | | "description": "Data are one of the most valuable products |
| | | curated by the Environmental Data Initiative (EDI). Data and metadata |
| | | derived from publicly funded research are made available through this |
| | | website with as few restrictions as possible, and on a |
| | | non-discriminatory basis. In return, EDI expects users of data to act |
| | | ethically by contacting the data provider prior to using it in any |
| | | published research. In accordance with professional etiquette, data |
| | | accessed from this website should be cited appropriately when used in |
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| | | "collection_procedures": "Well Design: Water table monitoring |
| | | wells are installed ~1 m below the baseflow water table. Wells are |
| | | constructed of 5 cm inner diameter PVC pipe with approximately 1 m |
| | | long, 0.25 mm slot screen lengths, capped at the bottom.Each site has |
| | | a network of five wells: A central well (C) and four wells ~40 m from |
| | | the center well in the four cardinal directions (N, S, E, W). Pressure |
| | | transducers to log water table levels at 30 minute intervals were |
| | | deployed in most of the wells at various times. Water Table Data:Site |
| | | data are listed by acronyms, see above, e.g., BDASn = Bosque del |
| | | Apache south site, north well. Variables include date, time, |
| | | groundwater temperature recorded by the transducer, if applicable (gw |
| | | temp, \u00b0C), depth to water table from grade at the well (DWT, cm), |
| | | water table elevation above sea level (WT elev, m, except for the |
| | | unsurveyed La Joya site), and a quality check (qc) column to indicate |
| | | estimated data (see below).Groundwater temperatures range from 8\u00b0 |
| | | to 20\u00b0 C with precision to the nearest tenth of a degree. Water |
| | | table levels range from 4 m depth to 0.5 m above the surface |
| | | (inundation) with precision to the nearest mm. Water table levels |
| | | collected with the following pressure transducers:1. Solinst model |
| | | 3001 LT M10 Leveloggers and model 3001 LT M1.5 Barologgers*, Solinst |
| | | Canada Ltd., Georgetown, ON, Canada.2. Schlumberger model DI501 Mini-, |
| | | model DI701 Cera-, and model DI501 Baro*-Divers, Schlumberger Water |
| | | Services,Tucson, AZ.3. EEI Submersible Sensor models 2.0 (2 m) and 5.0 |
| | | (4m), Electronic Engineering Innovations, Las Cruces, NM. These |
| | | transducers are vented (no barometric correction required) and do not |
| | | measure temperature.*Solinst and Schlumberger submersible transducers |
| | | measure total pressure (barometric and hydraulic). Barometric |
| | | transducers suspended above the water column in a well record |
| | | barometric pressure, which is subtracted from the total pressure |
| | | readings to arrive at hydraulic pressure, or well head.With all data |
| | | collections, well water levels are manually measured with a Solinst or |
| | | TestWell sounder and offset-corrected. Thirty-minute data missing |
| | | from a time series indicate that a logger was not deployed or a |
| | | malfunction occurred. Missing water table data are estimated in some |
| | | cases, especially when data are lost during the Apr 1 -- Nov 15 |
| | | growing season and at wells with long-term records. Estimates are |
| | | made by:1. The average rate of change within a time series from data |
| | | existing before and/or after the gap (e1 in the qc column).2. The |
| | | average rate of change from one or more nearby well logs during the |
| | | gap (e2 in the qc column).3. Linear regression with one or more of the |
| | | nearby well logs from data existing before and after the gap (e3 in |
| | | the qc column). Survey of location and elevation of wells:Survey data |
| | | collected by D. McDonnell, UNM Biology, Feb-Mar 2002, UTM NAD83. |
| | | Equipment loaned by University NAVSTAR Consortium (UNAVCO), Boulder, |
| | | CO. Equipment used: Trimble 4000 Receiver Systems (2) $24,000 Trimble |
| | | 4700 Reciever System (1) $8,000 Trimble Removable Groundplane Antennas |
| | | (3) $9,000 TSC-1 Controller (1) $5,000 Misc. ancillary equipment |
| | | $1,000 LARO site only: GPS data collected by J Thibault and J |
| | | Cleverly, UNM Biology. Garmin Etrex and Garmin III+, WGS 84. Data not |
| | | suitable for use in elev calculations at these wells. Coordinates and |
| | | c well elev are approximations.", |
| | | "collection_timeframe": "1999-2014", |
| | | "coordinate_system": "", |
| | | "created": "2023-04-27T19:10:41.403660", |
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| | | "data_source": "University of New Mexico", |
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| | | "datastore_active": false, |
| | | "description": "This study originated with the objective of |
| | | parameterizing riparian evapotranspiration (ET) in the water budget of |
| | | the middle Rio Grande of New Mexico. We hypothesized that flooding |
| | | and invasions of non-native species would impact the ecosystem's use |
| | | of water. Our objectives were to measure and compare the ET of native |
| | | (Rio Grande cottonwood, Populus deltoides ssp. wizleni) and non-native |
| | | (saltcedar, Tamarix chinensis, Russian olive, Eleagnus angustifolia) |
| | | bosque (woodland) communities and to evaluate how water use is |
| | | affected by climatic variability resulting in high river flows and |
| | | flooding as well as drought conditions and deep water tables. This |
| | | data set contains water table levels monitored at nine sites along the |
| | | Rio Grande riparian corridor between Albuquerque and Bosque del Apache |
| | | National Wildlife Refuge. Data date to 1999. Two sites remain active |
| | | and are well into their second decade of monitoring. One is in a |
| | | xero-riparian, non-flooding, saltcedar woodland within the Sevilleta |
| | | National Wildlife Refuge. The other is in a dense, monotypic |
| | | saltcedar thicket at the Bosque del Apache NWR that is subject to |
| | | flood pulses associated with high river flows. ", |
| | | "format": "HTML", |
| | | "geographic_location": "Description:\tThe northernmost group of |
| | | wells for SEV295 is at this location. Site Coordinates: Longitude |
| | | (degree): -106.6882 Latitude (degree): 35.126894", |
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| | | "name": "Groundwater Well Data from the Middle Rio Grande Valley |
| | | Riparian Zone, New Mexico (1999-2014)", |
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| | | "publish_method": "Data portal", |
| | | "quality_procedures": "", |
| | | "resource_contact_email": "[email protected]", |
| | | "resource_contact_name": "UNM Information Manager", |
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| | | "url": |
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| | | } |
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n | | n | "tags": [], |
| "title": "EDI Data Portal", | | "title": "EDI Data Portal", |
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t | "version": null | t | "version": "" |
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