Nitrogen isotope composition of ammonium and nitrate in bulk precipitation and forest throughfall (Record no. 51480)
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| 000 -LEADER | |
|---|---|
| fixed length control field | 02244nam a2200241Ia 4500 |
| 003 - CONTROL NUMBER IDENTIFIER | |
| control field | MX-MdCICY |
| 005 - DATE AND TIME OF LATEST TRANSACTION | |
| control field | 20250625160208.0 |
| 040 ## - CATALOGING SOURCE | |
| Transcribing agency | CICY |
| 090 ## - LOCALLY ASSIGNED LC-TYPE CALL NUMBER (OCLC); LOCAL CALL NUMBER (RLIN) | |
| Classification number (OCLC) (R) ; Classification number, CALL (RLIN) (NR) | B-17317 |
| 008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION | |
| fixed length control field | 250602s9999 xx |||||s2 |||| ||und|d |
| 245 10 - TITLE STATEMENT | |
| Title | Nitrogen isotope composition of ammonium and nitrate in bulk precipitation and forest throughfall |
| 490 0# - SERIES STATEMENT | |
| Volume/sequential designation | International Journal of Environmental Analytical Chemistry, 47(1), p.33-45, 1992 |
| 520 3# - SUMMARY, ETC. | |
| Summary, etc. | The stable nitrogen isotope composition of ammonium (NH4*)and nitrate (NO3)ions in bulk precipitation and forest throughfall was determined at Walker Branch watershed, a low elevation site (340 m)in northeastern Tennessee, and in cloud water from Whitetop Mountain, a high elevation site (1680 m)in southwestern Virginia. Tests of the method used indicated that sample processing did not introduce significant isotopic fractionation in measurements of nitrogen isotope composition. Mean ?15N values for NH4and NO3 -in solutions of artificial rain were within 0.3 per cento of the mean ?l5N values of nitrogen compounds used to make the solutions. Over a one-year period on Walker Branch watershed, the measured mean (±SD)?515N value for NH+ 4 in bulk precipitation and throughfall ( - 3.4 + 2.1 per cent0)was significantly less than that for N03( + 2.3±2.4 per cent0). The same relative pattern was observed in cloud water from Whitetop Mountain: mean (±SD)?15N in cloud water NH+4was - 5.5±3.2 per cent0;i.e., isotopically lighter than NO3 (+1.4±4.8 per cent0). The isotopic composition of NH+4in bulk precipitation and throughfall on Walker Branch watershed and in cloud water at Whitetop Mountain was consistent with origination through the washout of atmospheric NH3. However, the origins of NO3(gaseous versus aerosol precursors)could not be clearly established from ?5N measurements. |
| 650 14 - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| Topical term or geographic name entry element | BULK PRECIPITATION |
| 650 14 - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| Topical term or geographic name entry element | CLOUD WÁTER |
| 650 14 - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| Topical term or geographic name entry element | ION EXCHANGE |
| 650 14 - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| Topical term or geographic name entry element | NITROGEN-15 |
| 650 14 - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| Topical term or geographic name entry element | STABLE NITROGEN ISOTOPES |
| 650 14 - SUBJECT ADDED ENTRY--TOPICAL TERM | |
| Topical term or geographic name entry element | THROUGHFALL |
| 700 12 - ADDED ENTRY--PERSONAL NAME | |
| Personal name | Garten Jr, C. T. |
| 856 40 - ELECTRONIC LOCATION AND ACCESS | |
| Uniform Resource Identifier | <a href="https://drive.google.com/file/d/1HWuIVbZ6z8SL8cvbG6n0AYoNBIAXeGkk/view?usp=drivesdk">https://drive.google.com/file/d/1HWuIVbZ6z8SL8cvbG6n0AYoNBIAXeGkk/view?usp=drivesdk</a> |
| Public note | Para ver el documento ingresa a Google con tu cuenta: @cicy.edu.mx |
| 942 ## - ADDED ENTRY ELEMENTS (KOHA) | |
| Source of classification or shelving scheme | Clasificación local |
| Koha item type | Documentos solicitados |
| Lost status | Source of classification or shelving scheme | Damaged status | Not for loan | Collection | Home library | Current library | Shelving location | Date acquired | Total checkouts | Full call number | Date last seen | Price effective from | Koha item type |
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| Clasificación local | Ref1 | CICY | CICY | Documento préstamo interbibliotecario | 25.06.2025 | B-17317 | 25.06.2025 | 25.06.2025 | Documentos solicitados |
