Evaporation, infiltration and storage of soil water in different vegetation zones in the Qilian Mountains: a stable isotope perspective
<p<The processes of water storage have not been fully understood in different vegetation zones of mountainous areas, which is the main obstacle to further understanding hydrological processes and improving water resource assessments. To further understand the process of soil water movement in...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
G. Zhu [verfasserIn] L. Yong [verfasserIn] X. Zhao [verfasserIn] Y. Liu [verfasserIn] Z. Zhang [verfasserIn] Y. Xu [verfasserIn] Z. Sun [verfasserIn] L. Sang [verfasserIn] L. Wang [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2022 |
|---|
| Übergeordnetes Werk: |
In: Hydrology and Earth System Sciences - Copernicus Publications, 2005, 26(2022), Seite 3771-3784 |
|---|---|
| Übergeordnetes Werk: |
volume:26 ; year:2022 ; pages:3771-3784 |
| Links: |
Link aufrufen |
|---|
| DOI / URN: |
10.5194/hess-26-3771-2022 |
|---|
| Katalog-ID: |
DOAJ024858005 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | DOAJ024858005 | ||
| 003 | DE-627 | ||
| 005 | 20230501182437.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 230226s2022 xx |||||o 00| ||eng c | ||
| 024 | 7 | |a 10.5194/hess-26-3771-2022 |2 doi | |
| 035 | |a (DE-627)DOAJ024858005 | ||
| 035 | |a (DE-599)DOAJ506fb35dfc1d418e98cec2476251f3e4 | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 050 | 0 | |a TD1-1066 | |
| 050 | 0 | |a GE1-350 | |
| 100 | 0 | |a G. Zhu |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Evaporation, infiltration and storage of soil water in different vegetation zones in the Qilian Mountains: a stable isotope perspective |
| 264 | 1 | |c 2022 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a Computermedien |b c |2 rdamedia | ||
| 338 | |a Online-Ressource |b cr |2 rdacarrier | ||
| 520 | |a <p<The processes of water storage have not been fully understood in different vegetation zones of mountainous areas, which is the main obstacle to further understanding hydrological processes and improving water resource assessments. To further understand the process of soil water movement in different vegetation zones (alpine meadow (AM), coniferous forest (CF), mountain grassland (MG) and deciduous forest (DF)) of mountainous areas, this study monitored the temporal and spatial dynamics of hydrogen- and oxygen-stable isotopes in the precipitation and soil water of the Xiying River basin. The results show that the order of soil water evaporation intensities in the four vegetation zones was MG (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 3.4) <span class="inline-formula"<></span< DF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.1) <span class="inline-formula"<></span< CF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.7) <span class="inline-formula"<></span< AM (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 6.4). The soil water in the AM and CF evaporated from only the topsoil, and the rainfall input was fully mixed with each layer of soil. The evaporation signals of the MG and DF could penetrate deep into the middle and lower layers of the soil as precipitation quickly flowed into the deep soil through the soil matrix. Each vegetation zone's water storage capacity of the 0–40 cm soil layer followed the order of AM (46.9 mm) <span class="inline-formula"<></span< DF (33.0 mm) <span class="inline-formula"<></span< CF (32.1 mm) <span class="inline-formula"<></span< MG (20.3 mm). In addition, the 0–10 cm soil layer has the smallest soil water storage capacity (AM: 43.0 mm; CF: 28.0 mm; MG: 17.5 mm; DF: 29.1 mm). This work will provide a new reference for understanding soil hydrology in arid headwater areas.</p< | ||
| 653 | 0 | |a Technology | |
| 653 | 0 | |a T | |
| 653 | 0 | |a Environmental technology. Sanitary engineering | |
| 653 | 0 | |a Geography. Anthropology. Recreation | |
| 653 | 0 | |a G | |
| 653 | 0 | |a Environmental sciences | |
| 700 | 0 | |a G. Zhu |e verfasserin |4 aut | |
| 700 | 0 | |a L. Yong |e verfasserin |4 aut | |
| 700 | 0 | |a L. Yong |e verfasserin |4 aut | |
| 700 | 0 | |a X. Zhao |e verfasserin |4 aut | |
| 700 | 0 | |a X. Zhao |e verfasserin |4 aut | |
| 700 | 0 | |a Y. Liu |e verfasserin |4 aut | |
| 700 | 0 | |a Y. Liu |e verfasserin |4 aut | |
| 700 | 0 | |a Z. Zhang |e verfasserin |4 aut | |
| 700 | 0 | |a Z. Zhang |e verfasserin |4 aut | |
| 700 | 0 | |a Y. Xu |e verfasserin |4 aut | |
| 700 | 0 | |a Y. Xu |e verfasserin |4 aut | |
| 700 | 0 | |a Z. Sun |e verfasserin |4 aut | |
| 700 | 0 | |a Z. Sun |e verfasserin |4 aut | |
| 700 | 0 | |a L. Sang |e verfasserin |4 aut | |
| 700 | 0 | |a L. Sang |e verfasserin |4 aut | |
| 700 | 0 | |a L. Wang |e verfasserin |4 aut | |
| 700 | 0 | |a L. Wang |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i In |t Hydrology and Earth System Sciences |d Copernicus Publications, 2005 |g 26(2022), Seite 3771-3784 |w (DE-627)36277417X |w (DE-600)2100610-6 |x 16077938 |7 nnns |
| 773 | 1 | 8 | |g volume:26 |g year:2022 |g pages:3771-3784 |
| 856 | 4 | 0 | |u https://doi.org/10.5194/hess-26-3771-2022 |z kostenfrei |
| 856 | 4 | 0 | |u https://doaj.org/article/506fb35dfc1d418e98cec2476251f3e4 |z kostenfrei |
| 856 | 4 | 0 | |u https://hess.copernicus.org/articles/26/3771/2022/hess-26-3771-2022.pdf |z kostenfrei |
| 856 | 4 | 2 | |u https://doaj.org/toc/1027-5606 |y Journal toc |z kostenfrei |
| 856 | 4 | 2 | |u https://doaj.org/toc/1607-7938 |y Journal toc |z kostenfrei |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_DOAJ | ||
| 912 | |a SSG-OLC-PHA | ||
| 912 | |a GBV_ILN_11 | ||
| 912 | |a GBV_ILN_20 | ||
| 912 | |a GBV_ILN_22 | ||
| 912 | |a GBV_ILN_23 | ||
| 912 | |a GBV_ILN_24 | ||
| 912 | |a GBV_ILN_31 | ||
| 912 | |a GBV_ILN_39 | ||
| 912 | |a GBV_ILN_40 | ||
| 912 | |a GBV_ILN_60 | ||
| 912 | |a GBV_ILN_62 | ||
| 912 | |a GBV_ILN_63 | ||
| 912 | |a GBV_ILN_65 | ||
| 912 | |a GBV_ILN_69 | ||
| 912 | |a GBV_ILN_70 | ||
| 912 | |a GBV_ILN_73 | ||
| 912 | |a GBV_ILN_95 | ||
| 912 | |a GBV_ILN_105 | ||
| 912 | |a GBV_ILN_110 | ||
| 912 | |a GBV_ILN_151 | ||
| 912 | |a GBV_ILN_161 | ||
| 912 | |a GBV_ILN_170 | ||
| 912 | |a GBV_ILN_213 | ||
| 912 | |a GBV_ILN_230 | ||
| 912 | |a GBV_ILN_267 | ||
| 912 | |a GBV_ILN_285 | ||
| 912 | |a GBV_ILN_293 | ||
| 912 | |a GBV_ILN_370 | ||
| 912 | |a GBV_ILN_381 | ||
| 912 | |a GBV_ILN_602 | ||
| 912 | |a GBV_ILN_2003 | ||
| 912 | |a GBV_ILN_2014 | ||
| 912 | |a GBV_ILN_2147 | ||
| 912 | |a GBV_ILN_2148 | ||
| 912 | |a GBV_ILN_4012 | ||
| 912 | |a GBV_ILN_4037 | ||
| 912 | |a GBV_ILN_4112 | ||
| 912 | |a GBV_ILN_4125 | ||
| 912 | |a GBV_ILN_4126 | ||
| 912 | |a GBV_ILN_4249 | ||
| 912 | |a GBV_ILN_4305 | ||
| 912 | |a GBV_ILN_4306 | ||
| 912 | |a GBV_ILN_4307 | ||
| 912 | |a GBV_ILN_4313 | ||
| 912 | |a GBV_ILN_4322 | ||
| 912 | |a GBV_ILN_4323 | ||
| 912 | |a GBV_ILN_4324 | ||
| 912 | |a GBV_ILN_4325 | ||
| 912 | |a GBV_ILN_4335 | ||
| 912 | |a GBV_ILN_4338 | ||
| 912 | |a GBV_ILN_4367 | ||
| 912 | |a GBV_ILN_4700 | ||
| 951 | |a AR | ||
| 952 | |d 26 |j 2022 |h 3771-3784 | ||
| author_variant |
g z gz g z gz l y ly l y ly x z xz x z xz y l yl y l yl z z zz z z zz y x yx y x yx z s zs z s zs l s ls l s ls l w lw l w lw |
|---|---|
| matchkey_str |
article:16077938:2022----::vprtoiflrtoadtrgosiwtrnifrnvgttoznsnhqlamu |
| hierarchy_sort_str |
2022 |
| callnumber-subject-code |
TD |
| publishDate |
2022 |
| allfields |
10.5194/hess-26-3771-2022 doi (DE-627)DOAJ024858005 (DE-599)DOAJ506fb35dfc1d418e98cec2476251f3e4 DE-627 ger DE-627 rakwb eng TD1-1066 GE1-350 G. Zhu verfasserin aut Evaporation, infiltration and storage of soil water in different vegetation zones in the Qilian Mountains: a stable isotope perspective 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<The processes of water storage have not been fully understood in different vegetation zones of mountainous areas, which is the main obstacle to further understanding hydrological processes and improving water resource assessments. To further understand the process of soil water movement in different vegetation zones (alpine meadow (AM), coniferous forest (CF), mountain grassland (MG) and deciduous forest (DF)) of mountainous areas, this study monitored the temporal and spatial dynamics of hydrogen- and oxygen-stable isotopes in the precipitation and soil water of the Xiying River basin. The results show that the order of soil water evaporation intensities in the four vegetation zones was MG (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 3.4) <span class="inline-formula"<></span< DF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.1) <span class="inline-formula"<></span< CF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.7) <span class="inline-formula"<></span< AM (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 6.4). The soil water in the AM and CF evaporated from only the topsoil, and the rainfall input was fully mixed with each layer of soil. The evaporation signals of the MG and DF could penetrate deep into the middle and lower layers of the soil as precipitation quickly flowed into the deep soil through the soil matrix. Each vegetation zone's water storage capacity of the 0–40 cm soil layer followed the order of AM (46.9 mm) <span class="inline-formula"<></span< DF (33.0 mm) <span class="inline-formula"<></span< CF (32.1 mm) <span class="inline-formula"<></span< MG (20.3 mm). In addition, the 0–10 cm soil layer has the smallest soil water storage capacity (AM: 43.0 mm; CF: 28.0 mm; MG: 17.5 mm; DF: 29.1 mm). This work will provide a new reference for understanding soil hydrology in arid headwater areas.</p< Technology T Environmental technology. Sanitary engineering Geography. Anthropology. Recreation G Environmental sciences G. Zhu verfasserin aut L. Yong verfasserin aut L. Yong verfasserin aut X. Zhao verfasserin aut X. Zhao verfasserin aut Y. Liu verfasserin aut Y. Liu verfasserin aut Z. Zhang verfasserin aut Z. Zhang verfasserin aut Y. Xu verfasserin aut Y. Xu verfasserin aut Z. Sun verfasserin aut Z. Sun verfasserin aut L. Sang verfasserin aut L. Sang verfasserin aut L. Wang verfasserin aut L. Wang verfasserin aut In Hydrology and Earth System Sciences Copernicus Publications, 2005 26(2022), Seite 3771-3784 (DE-627)36277417X (DE-600)2100610-6 16077938 nnns volume:26 year:2022 pages:3771-3784 https://doi.org/10.5194/hess-26-3771-2022 kostenfrei https://doaj.org/article/506fb35dfc1d418e98cec2476251f3e4 kostenfrei https://hess.copernicus.org/articles/26/3771/2022/hess-26-3771-2022.pdf kostenfrei https://doaj.org/toc/1027-5606 Journal toc kostenfrei https://doaj.org/toc/1607-7938 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 26 2022 3771-3784 |
| spelling |
10.5194/hess-26-3771-2022 doi (DE-627)DOAJ024858005 (DE-599)DOAJ506fb35dfc1d418e98cec2476251f3e4 DE-627 ger DE-627 rakwb eng TD1-1066 GE1-350 G. Zhu verfasserin aut Evaporation, infiltration and storage of soil water in different vegetation zones in the Qilian Mountains: a stable isotope perspective 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<The processes of water storage have not been fully understood in different vegetation zones of mountainous areas, which is the main obstacle to further understanding hydrological processes and improving water resource assessments. To further understand the process of soil water movement in different vegetation zones (alpine meadow (AM), coniferous forest (CF), mountain grassland (MG) and deciduous forest (DF)) of mountainous areas, this study monitored the temporal and spatial dynamics of hydrogen- and oxygen-stable isotopes in the precipitation and soil water of the Xiying River basin. The results show that the order of soil water evaporation intensities in the four vegetation zones was MG (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 3.4) <span class="inline-formula"<></span< DF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.1) <span class="inline-formula"<></span< CF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.7) <span class="inline-formula"<></span< AM (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 6.4). The soil water in the AM and CF evaporated from only the topsoil, and the rainfall input was fully mixed with each layer of soil. The evaporation signals of the MG and DF could penetrate deep into the middle and lower layers of the soil as precipitation quickly flowed into the deep soil through the soil matrix. Each vegetation zone's water storage capacity of the 0–40 cm soil layer followed the order of AM (46.9 mm) <span class="inline-formula"<></span< DF (33.0 mm) <span class="inline-formula"<></span< CF (32.1 mm) <span class="inline-formula"<></span< MG (20.3 mm). In addition, the 0–10 cm soil layer has the smallest soil water storage capacity (AM: 43.0 mm; CF: 28.0 mm; MG: 17.5 mm; DF: 29.1 mm). This work will provide a new reference for understanding soil hydrology in arid headwater areas.</p< Technology T Environmental technology. Sanitary engineering Geography. Anthropology. Recreation G Environmental sciences G. Zhu verfasserin aut L. Yong verfasserin aut L. Yong verfasserin aut X. Zhao verfasserin aut X. Zhao verfasserin aut Y. Liu verfasserin aut Y. Liu verfasserin aut Z. Zhang verfasserin aut Z. Zhang verfasserin aut Y. Xu verfasserin aut Y. Xu verfasserin aut Z. Sun verfasserin aut Z. Sun verfasserin aut L. Sang verfasserin aut L. Sang verfasserin aut L. Wang verfasserin aut L. Wang verfasserin aut In Hydrology and Earth System Sciences Copernicus Publications, 2005 26(2022), Seite 3771-3784 (DE-627)36277417X (DE-600)2100610-6 16077938 nnns volume:26 year:2022 pages:3771-3784 https://doi.org/10.5194/hess-26-3771-2022 kostenfrei https://doaj.org/article/506fb35dfc1d418e98cec2476251f3e4 kostenfrei https://hess.copernicus.org/articles/26/3771/2022/hess-26-3771-2022.pdf kostenfrei https://doaj.org/toc/1027-5606 Journal toc kostenfrei https://doaj.org/toc/1607-7938 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 26 2022 3771-3784 |
| allfields_unstemmed |
10.5194/hess-26-3771-2022 doi (DE-627)DOAJ024858005 (DE-599)DOAJ506fb35dfc1d418e98cec2476251f3e4 DE-627 ger DE-627 rakwb eng TD1-1066 GE1-350 G. Zhu verfasserin aut Evaporation, infiltration and storage of soil water in different vegetation zones in the Qilian Mountains: a stable isotope perspective 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<The processes of water storage have not been fully understood in different vegetation zones of mountainous areas, which is the main obstacle to further understanding hydrological processes and improving water resource assessments. To further understand the process of soil water movement in different vegetation zones (alpine meadow (AM), coniferous forest (CF), mountain grassland (MG) and deciduous forest (DF)) of mountainous areas, this study monitored the temporal and spatial dynamics of hydrogen- and oxygen-stable isotopes in the precipitation and soil water of the Xiying River basin. The results show that the order of soil water evaporation intensities in the four vegetation zones was MG (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 3.4) <span class="inline-formula"<></span< DF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.1) <span class="inline-formula"<></span< CF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.7) <span class="inline-formula"<></span< AM (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 6.4). The soil water in the AM and CF evaporated from only the topsoil, and the rainfall input was fully mixed with each layer of soil. The evaporation signals of the MG and DF could penetrate deep into the middle and lower layers of the soil as precipitation quickly flowed into the deep soil through the soil matrix. Each vegetation zone's water storage capacity of the 0–40 cm soil layer followed the order of AM (46.9 mm) <span class="inline-formula"<></span< DF (33.0 mm) <span class="inline-formula"<></span< CF (32.1 mm) <span class="inline-formula"<></span< MG (20.3 mm). In addition, the 0–10 cm soil layer has the smallest soil water storage capacity (AM: 43.0 mm; CF: 28.0 mm; MG: 17.5 mm; DF: 29.1 mm). This work will provide a new reference for understanding soil hydrology in arid headwater areas.</p< Technology T Environmental technology. Sanitary engineering Geography. Anthropology. Recreation G Environmental sciences G. Zhu verfasserin aut L. Yong verfasserin aut L. Yong verfasserin aut X. Zhao verfasserin aut X. Zhao verfasserin aut Y. Liu verfasserin aut Y. Liu verfasserin aut Z. Zhang verfasserin aut Z. Zhang verfasserin aut Y. Xu verfasserin aut Y. Xu verfasserin aut Z. Sun verfasserin aut Z. Sun verfasserin aut L. Sang verfasserin aut L. Sang verfasserin aut L. Wang verfasserin aut L. Wang verfasserin aut In Hydrology and Earth System Sciences Copernicus Publications, 2005 26(2022), Seite 3771-3784 (DE-627)36277417X (DE-600)2100610-6 16077938 nnns volume:26 year:2022 pages:3771-3784 https://doi.org/10.5194/hess-26-3771-2022 kostenfrei https://doaj.org/article/506fb35dfc1d418e98cec2476251f3e4 kostenfrei https://hess.copernicus.org/articles/26/3771/2022/hess-26-3771-2022.pdf kostenfrei https://doaj.org/toc/1027-5606 Journal toc kostenfrei https://doaj.org/toc/1607-7938 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 26 2022 3771-3784 |
| allfieldsGer |
10.5194/hess-26-3771-2022 doi (DE-627)DOAJ024858005 (DE-599)DOAJ506fb35dfc1d418e98cec2476251f3e4 DE-627 ger DE-627 rakwb eng TD1-1066 GE1-350 G. Zhu verfasserin aut Evaporation, infiltration and storage of soil water in different vegetation zones in the Qilian Mountains: a stable isotope perspective 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<The processes of water storage have not been fully understood in different vegetation zones of mountainous areas, which is the main obstacle to further understanding hydrological processes and improving water resource assessments. To further understand the process of soil water movement in different vegetation zones (alpine meadow (AM), coniferous forest (CF), mountain grassland (MG) and deciduous forest (DF)) of mountainous areas, this study monitored the temporal and spatial dynamics of hydrogen- and oxygen-stable isotopes in the precipitation and soil water of the Xiying River basin. The results show that the order of soil water evaporation intensities in the four vegetation zones was MG (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 3.4) <span class="inline-formula"<></span< DF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.1) <span class="inline-formula"<></span< CF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.7) <span class="inline-formula"<></span< AM (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 6.4). The soil water in the AM and CF evaporated from only the topsoil, and the rainfall input was fully mixed with each layer of soil. The evaporation signals of the MG and DF could penetrate deep into the middle and lower layers of the soil as precipitation quickly flowed into the deep soil through the soil matrix. Each vegetation zone's water storage capacity of the 0–40 cm soil layer followed the order of AM (46.9 mm) <span class="inline-formula"<></span< DF (33.0 mm) <span class="inline-formula"<></span< CF (32.1 mm) <span class="inline-formula"<></span< MG (20.3 mm). In addition, the 0–10 cm soil layer has the smallest soil water storage capacity (AM: 43.0 mm; CF: 28.0 mm; MG: 17.5 mm; DF: 29.1 mm). This work will provide a new reference for understanding soil hydrology in arid headwater areas.</p< Technology T Environmental technology. Sanitary engineering Geography. Anthropology. Recreation G Environmental sciences G. Zhu verfasserin aut L. Yong verfasserin aut L. Yong verfasserin aut X. Zhao verfasserin aut X. Zhao verfasserin aut Y. Liu verfasserin aut Y. Liu verfasserin aut Z. Zhang verfasserin aut Z. Zhang verfasserin aut Y. Xu verfasserin aut Y. Xu verfasserin aut Z. Sun verfasserin aut Z. Sun verfasserin aut L. Sang verfasserin aut L. Sang verfasserin aut L. Wang verfasserin aut L. Wang verfasserin aut In Hydrology and Earth System Sciences Copernicus Publications, 2005 26(2022), Seite 3771-3784 (DE-627)36277417X (DE-600)2100610-6 16077938 nnns volume:26 year:2022 pages:3771-3784 https://doi.org/10.5194/hess-26-3771-2022 kostenfrei https://doaj.org/article/506fb35dfc1d418e98cec2476251f3e4 kostenfrei https://hess.copernicus.org/articles/26/3771/2022/hess-26-3771-2022.pdf kostenfrei https://doaj.org/toc/1027-5606 Journal toc kostenfrei https://doaj.org/toc/1607-7938 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 26 2022 3771-3784 |
| allfieldsSound |
10.5194/hess-26-3771-2022 doi (DE-627)DOAJ024858005 (DE-599)DOAJ506fb35dfc1d418e98cec2476251f3e4 DE-627 ger DE-627 rakwb eng TD1-1066 GE1-350 G. Zhu verfasserin aut Evaporation, infiltration and storage of soil water in different vegetation zones in the Qilian Mountains: a stable isotope perspective 2022 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<The processes of water storage have not been fully understood in different vegetation zones of mountainous areas, which is the main obstacle to further understanding hydrological processes and improving water resource assessments. To further understand the process of soil water movement in different vegetation zones (alpine meadow (AM), coniferous forest (CF), mountain grassland (MG) and deciduous forest (DF)) of mountainous areas, this study monitored the temporal and spatial dynamics of hydrogen- and oxygen-stable isotopes in the precipitation and soil water of the Xiying River basin. The results show that the order of soil water evaporation intensities in the four vegetation zones was MG (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 3.4) <span class="inline-formula"<></span< DF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.1) <span class="inline-formula"<></span< CF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.7) <span class="inline-formula"<></span< AM (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 6.4). The soil water in the AM and CF evaporated from only the topsoil, and the rainfall input was fully mixed with each layer of soil. The evaporation signals of the MG and DF could penetrate deep into the middle and lower layers of the soil as precipitation quickly flowed into the deep soil through the soil matrix. Each vegetation zone's water storage capacity of the 0–40 cm soil layer followed the order of AM (46.9 mm) <span class="inline-formula"<></span< DF (33.0 mm) <span class="inline-formula"<></span< CF (32.1 mm) <span class="inline-formula"<></span< MG (20.3 mm). In addition, the 0–10 cm soil layer has the smallest soil water storage capacity (AM: 43.0 mm; CF: 28.0 mm; MG: 17.5 mm; DF: 29.1 mm). This work will provide a new reference for understanding soil hydrology in arid headwater areas.</p< Technology T Environmental technology. Sanitary engineering Geography. Anthropology. Recreation G Environmental sciences G. Zhu verfasserin aut L. Yong verfasserin aut L. Yong verfasserin aut X. Zhao verfasserin aut X. Zhao verfasserin aut Y. Liu verfasserin aut Y. Liu verfasserin aut Z. Zhang verfasserin aut Z. Zhang verfasserin aut Y. Xu verfasserin aut Y. Xu verfasserin aut Z. Sun verfasserin aut Z. Sun verfasserin aut L. Sang verfasserin aut L. Sang verfasserin aut L. Wang verfasserin aut L. Wang verfasserin aut In Hydrology and Earth System Sciences Copernicus Publications, 2005 26(2022), Seite 3771-3784 (DE-627)36277417X (DE-600)2100610-6 16077938 nnns volume:26 year:2022 pages:3771-3784 https://doi.org/10.5194/hess-26-3771-2022 kostenfrei https://doaj.org/article/506fb35dfc1d418e98cec2476251f3e4 kostenfrei https://hess.copernicus.org/articles/26/3771/2022/hess-26-3771-2022.pdf kostenfrei https://doaj.org/toc/1027-5606 Journal toc kostenfrei https://doaj.org/toc/1607-7938 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 26 2022 3771-3784 |
| language |
English |
| source |
In Hydrology and Earth System Sciences 26(2022), Seite 3771-3784 volume:26 year:2022 pages:3771-3784 |
| sourceStr |
In Hydrology and Earth System Sciences 26(2022), Seite 3771-3784 volume:26 year:2022 pages:3771-3784 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Technology T Environmental technology. Sanitary engineering Geography. Anthropology. Recreation G Environmental sciences |
| isfreeaccess_bool |
true |
| container_title |
Hydrology and Earth System Sciences |
| authorswithroles_txt_mv |
G. Zhu @@aut@@ L. Yong @@aut@@ X. Zhao @@aut@@ Y. Liu @@aut@@ Z. Zhang @@aut@@ Y. Xu @@aut@@ Z. Sun @@aut@@ L. Sang @@aut@@ L. Wang @@aut@@ |
| publishDateDaySort_date |
2022-01-01T00:00:00Z |
| hierarchy_top_id |
36277417X |
| id |
DOAJ024858005 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">DOAJ024858005</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230501182437.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230226s2022 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.5194/hess-26-3771-2022</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ024858005</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJ506fb35dfc1d418e98cec2476251f3e4</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">TD1-1066</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">GE1-350</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">G. Zhu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Evaporation, infiltration and storage of soil water in different vegetation zones in the Qilian Mountains: a stable isotope perspective</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a"><p<The processes of water storage have not been fully understood in different vegetation zones of mountainous areas, which is the main obstacle to further understanding hydrological processes and improving water resource assessments. To further understand the process of soil water movement in different vegetation zones (alpine meadow (AM), coniferous forest (CF), mountain grassland (MG) and deciduous forest (DF)) of mountainous areas, this study monitored the temporal and spatial dynamics of hydrogen- and oxygen-stable isotopes in the precipitation and soil water of the Xiying River basin. The results show that the order of soil water evaporation intensities in the four vegetation zones was MG (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 3.4) <span class="inline-formula"<&gt;</span< DF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.1) <span class="inline-formula"<&gt;</span< CF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.7) <span class="inline-formula"<&gt;</span< AM (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 6.4). The soil water in the AM and CF evaporated from only the topsoil, and the rainfall input was fully mixed with each layer of soil. The evaporation signals of the MG and DF could penetrate deep into the middle and lower layers of the soil as precipitation quickly flowed into the deep soil through the soil matrix. Each vegetation zone's water storage capacity of the 0–40 cm soil layer followed the order of AM (46.9 mm) <span class="inline-formula"<&gt;</span< DF (33.0 mm) <span class="inline-formula"<&gt;</span< CF (32.1 mm) <span class="inline-formula"<&gt;</span< MG (20.3 mm). In addition, the 0–10 cm soil layer has the smallest soil water storage capacity (AM: 43.0 mm; CF: 28.0 mm; MG: 17.5 mm; DF: 29.1 mm). This work will provide a new reference for understanding soil hydrology in arid headwater areas.</p<</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Technology</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">T</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Environmental technology. Sanitary engineering</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Geography. Anthropology. Recreation</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">G</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Environmental sciences</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">G. Zhu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Yong</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Yong</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">X. Zhao</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">X. Zhao</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Y. Liu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Y. Liu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Z. Zhang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Z. Zhang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Y. Xu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Y. Xu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Z. Sun</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Z. Sun</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Sang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Sang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Wang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Wang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Hydrology and Earth System Sciences</subfield><subfield code="d">Copernicus Publications, 2005</subfield><subfield code="g">26(2022), Seite 3771-3784</subfield><subfield code="w">(DE-627)36277417X</subfield><subfield code="w">(DE-600)2100610-6</subfield><subfield code="x">16077938</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:26</subfield><subfield code="g">year:2022</subfield><subfield code="g">pages:3771-3784</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.5194/hess-26-3771-2022</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/506fb35dfc1d418e98cec2476251f3e4</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://hess.copernicus.org/articles/26/3771/2022/hess-26-3771-2022.pdf</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/1027-5606</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/1607-7938</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_170</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_267</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_381</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2147</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2148</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4335</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4367</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4700</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">26</subfield><subfield code="j">2022</subfield><subfield code="h">3771-3784</subfield></datafield></record></collection>
|
| callnumber-first |
T - Technology |
| author |
G. Zhu |
| spellingShingle |
G. Zhu misc TD1-1066 misc GE1-350 misc Technology misc T misc Environmental technology. Sanitary engineering misc Geography. Anthropology. Recreation misc G misc Environmental sciences Evaporation, infiltration and storage of soil water in different vegetation zones in the Qilian Mountains: a stable isotope perspective |
| authorStr |
G. Zhu |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)36277417X |
| format |
electronic Article |
| delete_txt_mv |
keep |
| author_role |
aut aut aut aut aut aut aut aut aut aut aut aut aut aut aut aut aut aut |
| collection |
DOAJ |
| remote_str |
true |
| callnumber-label |
TD1-1066 |
| illustrated |
Not Illustrated |
| issn |
16077938 |
| topic_title |
TD1-1066 GE1-350 Evaporation, infiltration and storage of soil water in different vegetation zones in the Qilian Mountains: a stable isotope perspective |
| topic |
misc TD1-1066 misc GE1-350 misc Technology misc T misc Environmental technology. Sanitary engineering misc Geography. Anthropology. Recreation misc G misc Environmental sciences |
| topic_unstemmed |
misc TD1-1066 misc GE1-350 misc Technology misc T misc Environmental technology. Sanitary engineering misc Geography. Anthropology. Recreation misc G misc Environmental sciences |
| topic_browse |
misc TD1-1066 misc GE1-350 misc Technology misc T misc Environmental technology. Sanitary engineering misc Geography. Anthropology. Recreation misc G misc Environmental sciences |
| format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
cr |
| hierarchy_parent_title |
Hydrology and Earth System Sciences |
| hierarchy_parent_id |
36277417X |
| hierarchy_top_title |
Hydrology and Earth System Sciences |
| isfreeaccess_txt |
true |
| familylinks_str_mv |
(DE-627)36277417X (DE-600)2100610-6 |
| title |
Evaporation, infiltration and storage of soil water in different vegetation zones in the Qilian Mountains: a stable isotope perspective |
| ctrlnum |
(DE-627)DOAJ024858005 (DE-599)DOAJ506fb35dfc1d418e98cec2476251f3e4 |
| title_full |
Evaporation, infiltration and storage of soil water in different vegetation zones in the Qilian Mountains: a stable isotope perspective |
| author_sort |
G. Zhu |
| journal |
Hydrology and Earth System Sciences |
| journalStr |
Hydrology and Earth System Sciences |
| callnumber-first-code |
T |
| lang_code |
eng |
| isOA_bool |
true |
| recordtype |
marc |
| publishDateSort |
2022 |
| contenttype_str_mv |
txt |
| container_start_page |
3771 |
| author_browse |
G. Zhu L. Yong X. Zhao Y. Liu Z. Zhang Y. Xu Z. Sun L. Sang L. Wang |
| container_volume |
26 |
| class |
TD1-1066 GE1-350 |
| format_se |
Elektronische Aufsätze |
| author-letter |
G. Zhu |
| doi_str_mv |
10.5194/hess-26-3771-2022 |
| author2-role |
verfasserin |
| title_sort |
evaporation, infiltration and storage of soil water in different vegetation zones in the qilian mountains: a stable isotope perspective |
| callnumber |
TD1-1066 |
| title_auth |
Evaporation, infiltration and storage of soil water in different vegetation zones in the Qilian Mountains: a stable isotope perspective |
| abstract |
<p<The processes of water storage have not been fully understood in different vegetation zones of mountainous areas, which is the main obstacle to further understanding hydrological processes and improving water resource assessments. To further understand the process of soil water movement in different vegetation zones (alpine meadow (AM), coniferous forest (CF), mountain grassland (MG) and deciduous forest (DF)) of mountainous areas, this study monitored the temporal and spatial dynamics of hydrogen- and oxygen-stable isotopes in the precipitation and soil water of the Xiying River basin. The results show that the order of soil water evaporation intensities in the four vegetation zones was MG (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 3.4) <span class="inline-formula"<></span< DF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.1) <span class="inline-formula"<></span< CF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.7) <span class="inline-formula"<></span< AM (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 6.4). The soil water in the AM and CF evaporated from only the topsoil, and the rainfall input was fully mixed with each layer of soil. The evaporation signals of the MG and DF could penetrate deep into the middle and lower layers of the soil as precipitation quickly flowed into the deep soil through the soil matrix. Each vegetation zone's water storage capacity of the 0–40 cm soil layer followed the order of AM (46.9 mm) <span class="inline-formula"<></span< DF (33.0 mm) <span class="inline-formula"<></span< CF (32.1 mm) <span class="inline-formula"<></span< MG (20.3 mm). In addition, the 0–10 cm soil layer has the smallest soil water storage capacity (AM: 43.0 mm; CF: 28.0 mm; MG: 17.5 mm; DF: 29.1 mm). This work will provide a new reference for understanding soil hydrology in arid headwater areas.</p< |
| abstractGer |
<p<The processes of water storage have not been fully understood in different vegetation zones of mountainous areas, which is the main obstacle to further understanding hydrological processes and improving water resource assessments. To further understand the process of soil water movement in different vegetation zones (alpine meadow (AM), coniferous forest (CF), mountain grassland (MG) and deciduous forest (DF)) of mountainous areas, this study monitored the temporal and spatial dynamics of hydrogen- and oxygen-stable isotopes in the precipitation and soil water of the Xiying River basin. The results show that the order of soil water evaporation intensities in the four vegetation zones was MG (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 3.4) <span class="inline-formula"<></span< DF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.1) <span class="inline-formula"<></span< CF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.7) <span class="inline-formula"<></span< AM (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 6.4). The soil water in the AM and CF evaporated from only the topsoil, and the rainfall input was fully mixed with each layer of soil. The evaporation signals of the MG and DF could penetrate deep into the middle and lower layers of the soil as precipitation quickly flowed into the deep soil through the soil matrix. Each vegetation zone's water storage capacity of the 0–40 cm soil layer followed the order of AM (46.9 mm) <span class="inline-formula"<></span< DF (33.0 mm) <span class="inline-formula"<></span< CF (32.1 mm) <span class="inline-formula"<></span< MG (20.3 mm). In addition, the 0–10 cm soil layer has the smallest soil water storage capacity (AM: 43.0 mm; CF: 28.0 mm; MG: 17.5 mm; DF: 29.1 mm). This work will provide a new reference for understanding soil hydrology in arid headwater areas.</p< |
| abstract_unstemmed |
<p<The processes of water storage have not been fully understood in different vegetation zones of mountainous areas, which is the main obstacle to further understanding hydrological processes and improving water resource assessments. To further understand the process of soil water movement in different vegetation zones (alpine meadow (AM), coniferous forest (CF), mountain grassland (MG) and deciduous forest (DF)) of mountainous areas, this study monitored the temporal and spatial dynamics of hydrogen- and oxygen-stable isotopes in the precipitation and soil water of the Xiying River basin. The results show that the order of soil water evaporation intensities in the four vegetation zones was MG (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 3.4) <span class="inline-formula"<></span< DF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.1) <span class="inline-formula"<></span< CF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.7) <span class="inline-formula"<></span< AM (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 6.4). The soil water in the AM and CF evaporated from only the topsoil, and the rainfall input was fully mixed with each layer of soil. The evaporation signals of the MG and DF could penetrate deep into the middle and lower layers of the soil as precipitation quickly flowed into the deep soil through the soil matrix. Each vegetation zone's water storage capacity of the 0–40 cm soil layer followed the order of AM (46.9 mm) <span class="inline-formula"<></span< DF (33.0 mm) <span class="inline-formula"<></span< CF (32.1 mm) <span class="inline-formula"<></span< MG (20.3 mm). In addition, the 0–10 cm soil layer has the smallest soil water storage capacity (AM: 43.0 mm; CF: 28.0 mm; MG: 17.5 mm; DF: 29.1 mm). This work will provide a new reference for understanding soil hydrology in arid headwater areas.</p< |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ SSG-OLC-PHA GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 |
| title_short |
Evaporation, infiltration and storage of soil water in different vegetation zones in the Qilian Mountains: a stable isotope perspective |
| url |
https://doi.org/10.5194/hess-26-3771-2022 https://doaj.org/article/506fb35dfc1d418e98cec2476251f3e4 https://hess.copernicus.org/articles/26/3771/2022/hess-26-3771-2022.pdf https://doaj.org/toc/1027-5606 https://doaj.org/toc/1607-7938 |
| remote_bool |
true |
| author2 |
G. Zhu L. Yong X. Zhao Y. Liu Z. Zhang Y. Xu Z. Sun L. Sang L. Wang |
| author2Str |
G. Zhu L. Yong X. Zhao Y. Liu Z. Zhang Y. Xu Z. Sun L. Sang L. Wang |
| ppnlink |
36277417X |
| callnumber-subject |
TD - Environmental Technology |
| mediatype_str_mv |
c |
| isOA_txt |
true |
| hochschulschrift_bool |
false |
| doi_str |
10.5194/hess-26-3771-2022 |
| callnumber-a |
TD1-1066 |
| up_date |
2024-07-04T00:39:41.060Z |
| _version_ |
1803606903814619136 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">DOAJ024858005</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230501182437.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230226s2022 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.5194/hess-26-3771-2022</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)DOAJ024858005</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)DOAJ506fb35dfc1d418e98cec2476251f3e4</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">TD1-1066</subfield></datafield><datafield tag="050" ind1=" " ind2="0"><subfield code="a">GE1-350</subfield></datafield><datafield tag="100" ind1="0" ind2=" "><subfield code="a">G. Zhu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Evaporation, infiltration and storage of soil water in different vegetation zones in the Qilian Mountains: a stable isotope perspective</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a"><p<The processes of water storage have not been fully understood in different vegetation zones of mountainous areas, which is the main obstacle to further understanding hydrological processes and improving water resource assessments. To further understand the process of soil water movement in different vegetation zones (alpine meadow (AM), coniferous forest (CF), mountain grassland (MG) and deciduous forest (DF)) of mountainous areas, this study monitored the temporal and spatial dynamics of hydrogen- and oxygen-stable isotopes in the precipitation and soil water of the Xiying River basin. The results show that the order of soil water evaporation intensities in the four vegetation zones was MG (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 3.4) <span class="inline-formula"<&gt;</span< DF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.1) <span class="inline-formula"<&gt;</span< CF (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 4.7) <span class="inline-formula"<&gt;</span< AM (SWL<span class="inline-formula"<<sub<slop</sub<</span<: 6.4). The soil water in the AM and CF evaporated from only the topsoil, and the rainfall input was fully mixed with each layer of soil. The evaporation signals of the MG and DF could penetrate deep into the middle and lower layers of the soil as precipitation quickly flowed into the deep soil through the soil matrix. Each vegetation zone's water storage capacity of the 0–40 cm soil layer followed the order of AM (46.9 mm) <span class="inline-formula"<&gt;</span< DF (33.0 mm) <span class="inline-formula"<&gt;</span< CF (32.1 mm) <span class="inline-formula"<&gt;</span< MG (20.3 mm). In addition, the 0–10 cm soil layer has the smallest soil water storage capacity (AM: 43.0 mm; CF: 28.0 mm; MG: 17.5 mm; DF: 29.1 mm). This work will provide a new reference for understanding soil hydrology in arid headwater areas.</p<</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Technology</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">T</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Environmental technology. Sanitary engineering</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Geography. Anthropology. Recreation</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">G</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Environmental sciences</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">G. Zhu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Yong</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Yong</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">X. Zhao</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">X. Zhao</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Y. Liu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Y. Liu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Z. Zhang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Z. Zhang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Y. Xu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Y. Xu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Z. Sun</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">Z. Sun</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Sang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Sang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Wang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">L. Wang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">Hydrology and Earth System Sciences</subfield><subfield code="d">Copernicus Publications, 2005</subfield><subfield code="g">26(2022), Seite 3771-3784</subfield><subfield code="w">(DE-627)36277417X</subfield><subfield code="w">(DE-600)2100610-6</subfield><subfield code="x">16077938</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:26</subfield><subfield code="g">year:2022</subfield><subfield code="g">pages:3771-3784</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.5194/hess-26-3771-2022</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/506fb35dfc1d418e98cec2476251f3e4</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://hess.copernicus.org/articles/26/3771/2022/hess-26-3771-2022.pdf</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/1027-5606</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/1607-7938</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_39</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_170</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_213</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_230</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_267</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_285</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_381</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2147</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2148</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4012</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4249</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4306</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4307</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4322</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4325</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4335</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4367</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4700</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">26</subfield><subfield code="j">2022</subfield><subfield code="h">3771-3784</subfield></datafield></record></collection>
|
| score |
7.3990517 |