Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes
Abstract Subsurface-water flow pathways in three different land-use areas (non-irrigated grassland, poplar forest, and irrigated arable land) in the central North China Plain were investigated using oxygen (18O) and hydrogen (2H) isotopes in samples of precipitation, soils, and groundwater. Soil wat...
Ausführliche Beschreibung
Autor*in: |
Ma, Bin [verfasserIn] |
---|
Format: |
Artikel |
---|---|
Sprache: |
Englisch |
Erschienen: |
2017 |
---|
Schlagwörter: |
---|
Anmerkung: |
© Springer-Verlag Berlin Heidelberg 2017 |
---|
Übergeordnetes Werk: |
Enthalten in: Hydrogeology journal - Springer Berlin Heidelberg, 1995, 25(2017), 3 vom: 07. Jan., Seite 675-688 |
---|---|
Übergeordnetes Werk: |
volume:25 ; year:2017 ; number:3 ; day:07 ; month:01 ; pages:675-688 |
Links: |
---|
DOI / URN: |
10.1007/s10040-016-1525-5 |
---|
Katalog-ID: |
OLC2040028307 |
---|
LEADER | 01000caa a22002652 4500 | ||
---|---|---|---|
001 | OLC2040028307 | ||
003 | DE-627 | ||
005 | 20230502161125.0 | ||
007 | tu | ||
008 | 200819s2017 xx ||||| 00| ||eng c | ||
024 | 7 | |a 10.1007/s10040-016-1525-5 |2 doi | |
035 | |a (DE-627)OLC2040028307 | ||
035 | |a (DE-He213)s10040-016-1525-5-p | ||
040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
041 | |a eng | ||
082 | 0 | 4 | |a 550 |q VZ |
082 | 0 | 4 | |a 550 |q VZ |
084 | |a 13 |2 ssgn | ||
100 | 1 | |a Ma, Bin |e verfasserin |4 aut | |
245 | 1 | 0 | |a Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes |
264 | 1 | |c 2017 | |
336 | |a Text |b txt |2 rdacontent | ||
337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
338 | |a Band |b nc |2 rdacarrier | ||
500 | |a © Springer-Verlag Berlin Heidelberg 2017 | ||
520 | |a Abstract Subsurface-water flow pathways in three different land-use areas (non-irrigated grassland, poplar forest, and irrigated arable land) in the central North China Plain were investigated using oxygen (18O) and hydrogen (2H) isotopes in samples of precipitation, soils, and groundwater. Soil water in the top 10 cm was significantly affected by both evaporation and infiltration. Water at 10–40 cm depth in the grassland and arable land, and 10–60 cm in poplar forest, showed a relatively short residence time, as a substantial proportion of antecedent soil water was mixed with a 92-mm storm infiltration event, whereas below those depths (down to 150 cm), depleted $ δ^{18} $O spikes suggested that some storm water bypassed the shallow soil layers. Significant differences, in soil-water content and $ δ^{18} $O values, within a small area, suggested that the proportion of immobile soil water and water flowing in subsurface pathways varies depending on local vegetation cover, soil characteristics and irrigation applications. Soil-water $ δ^{18} $O values revealed that preferential flow and diffuse flow coexist. Preferential flow was active within the root zone, independent of antecedent soil-water content, in both poplar forest and arable land, whereas diffuse flow was observed in grassland. The depleted $ δ^{18} $O spikes at 20–50 cm depth in the arable land suggested the infiltration of irrigation water during the dry season. Temporal isotopic variations in precipitation were subdued in the shallow groundwater, suggesting more complete mixing of different input waters in the unsaturated zone before reaching the shallow groundwater. | ||
650 | 4 | |a Stable isotopes | |
650 | 4 | |a Unsaturated zone | |
650 | 4 | |a Diffuse flow | |
650 | 4 | |a Preferential flow | |
650 | 4 | |a China | |
700 | 1 | |a Liang, Xing |4 aut | |
700 | 1 | |a Liu, Shaohua |4 aut | |
700 | 1 | |a Jin, Menggui |4 aut | |
700 | 1 | |a Nimmo, John R. |4 aut | |
700 | 1 | |a Li, Jing |4 aut | |
773 | 0 | 8 | |i Enthalten in |t Hydrogeology journal |d Springer Berlin Heidelberg, 1995 |g 25(2017), 3 vom: 07. Jan., Seite 675-688 |w (DE-627)18393735X |w (DE-600)1227482-3 |w (DE-576)045314829 |x 1431-2174 |7 nnns |
773 | 1 | 8 | |g volume:25 |g year:2017 |g number:3 |g day:07 |g month:01 |g pages:675-688 |
856 | 4 | 1 | |u https://doi.org/10.1007/s10040-016-1525-5 |z lizenzpflichtig |3 Volltext |
912 | |a GBV_USEFLAG_A | ||
912 | |a SYSFLAG_A | ||
912 | |a GBV_OLC | ||
912 | |a SSG-OLC-GEO | ||
912 | |a SSG-OPC-GGO | ||
912 | |a GBV_ILN_70 | ||
912 | |a GBV_ILN_183 | ||
912 | |a GBV_ILN_267 | ||
912 | |a GBV_ILN_2018 | ||
912 | |a GBV_ILN_4046 | ||
912 | |a GBV_ILN_4112 | ||
912 | |a GBV_ILN_4277 | ||
951 | |a AR | ||
952 | |d 25 |j 2017 |e 3 |b 07 |c 01 |h 675-688 |
author_variant |
b m bm x l xl s l sl m j mj j r n jr jrn j l jl |
---|---|
matchkey_str |
article:14312174:2017----::vlainfifsadrfrnillwahasfnitaepeiiainnirgto |
hierarchy_sort_str |
2017 |
publishDate |
2017 |
allfields |
10.1007/s10040-016-1525-5 doi (DE-627)OLC2040028307 (DE-He213)s10040-016-1525-5-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Ma, Bin verfasserin aut Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Berlin Heidelberg 2017 Abstract Subsurface-water flow pathways in three different land-use areas (non-irrigated grassland, poplar forest, and irrigated arable land) in the central North China Plain were investigated using oxygen (18O) and hydrogen (2H) isotopes in samples of precipitation, soils, and groundwater. Soil water in the top 10 cm was significantly affected by both evaporation and infiltration. Water at 10–40 cm depth in the grassland and arable land, and 10–60 cm in poplar forest, showed a relatively short residence time, as a substantial proportion of antecedent soil water was mixed with a 92-mm storm infiltration event, whereas below those depths (down to 150 cm), depleted $ δ^{18} $O spikes suggested that some storm water bypassed the shallow soil layers. Significant differences, in soil-water content and $ δ^{18} $O values, within a small area, suggested that the proportion of immobile soil water and water flowing in subsurface pathways varies depending on local vegetation cover, soil characteristics and irrigation applications. Soil-water $ δ^{18} $O values revealed that preferential flow and diffuse flow coexist. Preferential flow was active within the root zone, independent of antecedent soil-water content, in both poplar forest and arable land, whereas diffuse flow was observed in grassland. The depleted $ δ^{18} $O spikes at 20–50 cm depth in the arable land suggested the infiltration of irrigation water during the dry season. Temporal isotopic variations in precipitation were subdued in the shallow groundwater, suggesting more complete mixing of different input waters in the unsaturated zone before reaching the shallow groundwater. Stable isotopes Unsaturated zone Diffuse flow Preferential flow China Liang, Xing aut Liu, Shaohua aut Jin, Menggui aut Nimmo, John R. aut Li, Jing aut Enthalten in Hydrogeology journal Springer Berlin Heidelberg, 1995 25(2017), 3 vom: 07. Jan., Seite 675-688 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:25 year:2017 number:3 day:07 month:01 pages:675-688 https://doi.org/10.1007/s10040-016-1525-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_183 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4277 AR 25 2017 3 07 01 675-688 |
spelling |
10.1007/s10040-016-1525-5 doi (DE-627)OLC2040028307 (DE-He213)s10040-016-1525-5-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Ma, Bin verfasserin aut Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Berlin Heidelberg 2017 Abstract Subsurface-water flow pathways in three different land-use areas (non-irrigated grassland, poplar forest, and irrigated arable land) in the central North China Plain were investigated using oxygen (18O) and hydrogen (2H) isotopes in samples of precipitation, soils, and groundwater. Soil water in the top 10 cm was significantly affected by both evaporation and infiltration. Water at 10–40 cm depth in the grassland and arable land, and 10–60 cm in poplar forest, showed a relatively short residence time, as a substantial proportion of antecedent soil water was mixed with a 92-mm storm infiltration event, whereas below those depths (down to 150 cm), depleted $ δ^{18} $O spikes suggested that some storm water bypassed the shallow soil layers. Significant differences, in soil-water content and $ δ^{18} $O values, within a small area, suggested that the proportion of immobile soil water and water flowing in subsurface pathways varies depending on local vegetation cover, soil characteristics and irrigation applications. Soil-water $ δ^{18} $O values revealed that preferential flow and diffuse flow coexist. Preferential flow was active within the root zone, independent of antecedent soil-water content, in both poplar forest and arable land, whereas diffuse flow was observed in grassland. The depleted $ δ^{18} $O spikes at 20–50 cm depth in the arable land suggested the infiltration of irrigation water during the dry season. Temporal isotopic variations in precipitation were subdued in the shallow groundwater, suggesting more complete mixing of different input waters in the unsaturated zone before reaching the shallow groundwater. Stable isotopes Unsaturated zone Diffuse flow Preferential flow China Liang, Xing aut Liu, Shaohua aut Jin, Menggui aut Nimmo, John R. aut Li, Jing aut Enthalten in Hydrogeology journal Springer Berlin Heidelberg, 1995 25(2017), 3 vom: 07. Jan., Seite 675-688 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:25 year:2017 number:3 day:07 month:01 pages:675-688 https://doi.org/10.1007/s10040-016-1525-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_183 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4277 AR 25 2017 3 07 01 675-688 |
allfields_unstemmed |
10.1007/s10040-016-1525-5 doi (DE-627)OLC2040028307 (DE-He213)s10040-016-1525-5-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Ma, Bin verfasserin aut Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Berlin Heidelberg 2017 Abstract Subsurface-water flow pathways in three different land-use areas (non-irrigated grassland, poplar forest, and irrigated arable land) in the central North China Plain were investigated using oxygen (18O) and hydrogen (2H) isotopes in samples of precipitation, soils, and groundwater. Soil water in the top 10 cm was significantly affected by both evaporation and infiltration. Water at 10–40 cm depth in the grassland and arable land, and 10–60 cm in poplar forest, showed a relatively short residence time, as a substantial proportion of antecedent soil water was mixed with a 92-mm storm infiltration event, whereas below those depths (down to 150 cm), depleted $ δ^{18} $O spikes suggested that some storm water bypassed the shallow soil layers. Significant differences, in soil-water content and $ δ^{18} $O values, within a small area, suggested that the proportion of immobile soil water and water flowing in subsurface pathways varies depending on local vegetation cover, soil characteristics and irrigation applications. Soil-water $ δ^{18} $O values revealed that preferential flow and diffuse flow coexist. Preferential flow was active within the root zone, independent of antecedent soil-water content, in both poplar forest and arable land, whereas diffuse flow was observed in grassland. The depleted $ δ^{18} $O spikes at 20–50 cm depth in the arable land suggested the infiltration of irrigation water during the dry season. Temporal isotopic variations in precipitation were subdued in the shallow groundwater, suggesting more complete mixing of different input waters in the unsaturated zone before reaching the shallow groundwater. Stable isotopes Unsaturated zone Diffuse flow Preferential flow China Liang, Xing aut Liu, Shaohua aut Jin, Menggui aut Nimmo, John R. aut Li, Jing aut Enthalten in Hydrogeology journal Springer Berlin Heidelberg, 1995 25(2017), 3 vom: 07. Jan., Seite 675-688 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:25 year:2017 number:3 day:07 month:01 pages:675-688 https://doi.org/10.1007/s10040-016-1525-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_183 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4277 AR 25 2017 3 07 01 675-688 |
allfieldsGer |
10.1007/s10040-016-1525-5 doi (DE-627)OLC2040028307 (DE-He213)s10040-016-1525-5-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Ma, Bin verfasserin aut Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Berlin Heidelberg 2017 Abstract Subsurface-water flow pathways in three different land-use areas (non-irrigated grassland, poplar forest, and irrigated arable land) in the central North China Plain were investigated using oxygen (18O) and hydrogen (2H) isotopes in samples of precipitation, soils, and groundwater. Soil water in the top 10 cm was significantly affected by both evaporation and infiltration. Water at 10–40 cm depth in the grassland and arable land, and 10–60 cm in poplar forest, showed a relatively short residence time, as a substantial proportion of antecedent soil water was mixed with a 92-mm storm infiltration event, whereas below those depths (down to 150 cm), depleted $ δ^{18} $O spikes suggested that some storm water bypassed the shallow soil layers. Significant differences, in soil-water content and $ δ^{18} $O values, within a small area, suggested that the proportion of immobile soil water and water flowing in subsurface pathways varies depending on local vegetation cover, soil characteristics and irrigation applications. Soil-water $ δ^{18} $O values revealed that preferential flow and diffuse flow coexist. Preferential flow was active within the root zone, independent of antecedent soil-water content, in both poplar forest and arable land, whereas diffuse flow was observed in grassland. The depleted $ δ^{18} $O spikes at 20–50 cm depth in the arable land suggested the infiltration of irrigation water during the dry season. Temporal isotopic variations in precipitation were subdued in the shallow groundwater, suggesting more complete mixing of different input waters in the unsaturated zone before reaching the shallow groundwater. Stable isotopes Unsaturated zone Diffuse flow Preferential flow China Liang, Xing aut Liu, Shaohua aut Jin, Menggui aut Nimmo, John R. aut Li, Jing aut Enthalten in Hydrogeology journal Springer Berlin Heidelberg, 1995 25(2017), 3 vom: 07. Jan., Seite 675-688 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:25 year:2017 number:3 day:07 month:01 pages:675-688 https://doi.org/10.1007/s10040-016-1525-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_183 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4277 AR 25 2017 3 07 01 675-688 |
allfieldsSound |
10.1007/s10040-016-1525-5 doi (DE-627)OLC2040028307 (DE-He213)s10040-016-1525-5-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Ma, Bin verfasserin aut Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes 2017 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag Berlin Heidelberg 2017 Abstract Subsurface-water flow pathways in three different land-use areas (non-irrigated grassland, poplar forest, and irrigated arable land) in the central North China Plain were investigated using oxygen (18O) and hydrogen (2H) isotopes in samples of precipitation, soils, and groundwater. Soil water in the top 10 cm was significantly affected by both evaporation and infiltration. Water at 10–40 cm depth in the grassland and arable land, and 10–60 cm in poplar forest, showed a relatively short residence time, as a substantial proportion of antecedent soil water was mixed with a 92-mm storm infiltration event, whereas below those depths (down to 150 cm), depleted $ δ^{18} $O spikes suggested that some storm water bypassed the shallow soil layers. Significant differences, in soil-water content and $ δ^{18} $O values, within a small area, suggested that the proportion of immobile soil water and water flowing in subsurface pathways varies depending on local vegetation cover, soil characteristics and irrigation applications. Soil-water $ δ^{18} $O values revealed that preferential flow and diffuse flow coexist. Preferential flow was active within the root zone, independent of antecedent soil-water content, in both poplar forest and arable land, whereas diffuse flow was observed in grassland. The depleted $ δ^{18} $O spikes at 20–50 cm depth in the arable land suggested the infiltration of irrigation water during the dry season. Temporal isotopic variations in precipitation were subdued in the shallow groundwater, suggesting more complete mixing of different input waters in the unsaturated zone before reaching the shallow groundwater. Stable isotopes Unsaturated zone Diffuse flow Preferential flow China Liang, Xing aut Liu, Shaohua aut Jin, Menggui aut Nimmo, John R. aut Li, Jing aut Enthalten in Hydrogeology journal Springer Berlin Heidelberg, 1995 25(2017), 3 vom: 07. Jan., Seite 675-688 (DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 1431-2174 nnns volume:25 year:2017 number:3 day:07 month:01 pages:675-688 https://doi.org/10.1007/s10040-016-1525-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_183 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4277 AR 25 2017 3 07 01 675-688 |
language |
English |
source |
Enthalten in Hydrogeology journal 25(2017), 3 vom: 07. Jan., Seite 675-688 volume:25 year:2017 number:3 day:07 month:01 pages:675-688 |
sourceStr |
Enthalten in Hydrogeology journal 25(2017), 3 vom: 07. Jan., Seite 675-688 volume:25 year:2017 number:3 day:07 month:01 pages:675-688 |
format_phy_str_mv |
Article |
institution |
findex.gbv.de |
topic_facet |
Stable isotopes Unsaturated zone Diffuse flow Preferential flow China |
dewey-raw |
550 |
isfreeaccess_bool |
false |
container_title |
Hydrogeology journal |
authorswithroles_txt_mv |
Ma, Bin @@aut@@ Liang, Xing @@aut@@ Liu, Shaohua @@aut@@ Jin, Menggui @@aut@@ Nimmo, John R. @@aut@@ Li, Jing @@aut@@ |
publishDateDaySort_date |
2017-01-07T00:00:00Z |
hierarchy_top_id |
18393735X |
dewey-sort |
3550 |
id |
OLC2040028307 |
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">OLC2040028307</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230502161125.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2017 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10040-016-1525-5</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2040028307</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s10040-016-1525-5-p</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="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Ma, Bin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2017</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">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag Berlin Heidelberg 2017</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Subsurface-water flow pathways in three different land-use areas (non-irrigated grassland, poplar forest, and irrigated arable land) in the central North China Plain were investigated using oxygen (18O) and hydrogen (2H) isotopes in samples of precipitation, soils, and groundwater. Soil water in the top 10 cm was significantly affected by both evaporation and infiltration. Water at 10–40 cm depth in the grassland and arable land, and 10–60 cm in poplar forest, showed a relatively short residence time, as a substantial proportion of antecedent soil water was mixed with a 92-mm storm infiltration event, whereas below those depths (down to 150 cm), depleted $ δ^{18} $O spikes suggested that some storm water bypassed the shallow soil layers. Significant differences, in soil-water content and $ δ^{18} $O values, within a small area, suggested that the proportion of immobile soil water and water flowing in subsurface pathways varies depending on local vegetation cover, soil characteristics and irrigation applications. Soil-water $ δ^{18} $O values revealed that preferential flow and diffuse flow coexist. Preferential flow was active within the root zone, independent of antecedent soil-water content, in both poplar forest and arable land, whereas diffuse flow was observed in grassland. The depleted $ δ^{18} $O spikes at 20–50 cm depth in the arable land suggested the infiltration of irrigation water during the dry season. Temporal isotopic variations in precipitation were subdued in the shallow groundwater, suggesting more complete mixing of different input waters in the unsaturated zone before reaching the shallow groundwater.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Stable isotopes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Unsaturated zone</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Diffuse flow</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Preferential flow</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">China</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liang, Xing</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liu, Shaohua</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jin, Menggui</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Nimmo, John R.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Li, Jing</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Hydrogeology journal</subfield><subfield code="d">Springer Berlin Heidelberg, 1995</subfield><subfield code="g">25(2017), 3 vom: 07. Jan., Seite 675-688</subfield><subfield code="w">(DE-627)18393735X</subfield><subfield code="w">(DE-600)1227482-3</subfield><subfield code="w">(DE-576)045314829</subfield><subfield code="x">1431-2174</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:25</subfield><subfield code="g">year:2017</subfield><subfield code="g">number:3</subfield><subfield code="g">day:07</subfield><subfield code="g">month:01</subfield><subfield code="g">pages:675-688</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s10040-016-1525-5</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</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_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</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_183</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_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4046</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_4277</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">25</subfield><subfield code="j">2017</subfield><subfield code="e">3</subfield><subfield code="b">07</subfield><subfield code="c">01</subfield><subfield code="h">675-688</subfield></datafield></record></collection>
|
author |
Ma, Bin |
spellingShingle |
Ma, Bin ddc 550 ssgn 13 misc Stable isotopes misc Unsaturated zone misc Diffuse flow misc Preferential flow misc China Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes |
authorStr |
Ma, Bin |
ppnlink_with_tag_str_mv |
@@773@@(DE-627)18393735X |
format |
Article |
dewey-ones |
550 - Earth sciences |
delete_txt_mv |
keep |
author_role |
aut aut aut aut aut aut |
collection |
OLC |
remote_str |
false |
illustrated |
Not Illustrated |
issn |
1431-2174 |
topic_title |
550 VZ 13 ssgn Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes Stable isotopes Unsaturated zone Diffuse flow Preferential flow China |
topic |
ddc 550 ssgn 13 misc Stable isotopes misc Unsaturated zone misc Diffuse flow misc Preferential flow misc China |
topic_unstemmed |
ddc 550 ssgn 13 misc Stable isotopes misc Unsaturated zone misc Diffuse flow misc Preferential flow misc China |
topic_browse |
ddc 550 ssgn 13 misc Stable isotopes misc Unsaturated zone misc Diffuse flow misc Preferential flow misc China |
format_facet |
Aufsätze Gedruckte Aufsätze |
format_main_str_mv |
Text Zeitschrift/Artikel |
carriertype_str_mv |
nc |
hierarchy_parent_title |
Hydrogeology journal |
hierarchy_parent_id |
18393735X |
dewey-tens |
550 - Earth sciences & geology |
hierarchy_top_title |
Hydrogeology journal |
isfreeaccess_txt |
false |
familylinks_str_mv |
(DE-627)18393735X (DE-600)1227482-3 (DE-576)045314829 |
title |
Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes |
ctrlnum |
(DE-627)OLC2040028307 (DE-He213)s10040-016-1525-5-p |
title_full |
Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes |
author_sort |
Ma, Bin |
journal |
Hydrogeology journal |
journalStr |
Hydrogeology journal |
lang_code |
eng |
isOA_bool |
false |
dewey-hundreds |
500 - Science |
recordtype |
marc |
publishDateSort |
2017 |
contenttype_str_mv |
txt |
container_start_page |
675 |
author_browse |
Ma, Bin Liang, Xing Liu, Shaohua Jin, Menggui Nimmo, John R. Li, Jing |
container_volume |
25 |
class |
550 VZ 13 ssgn |
format_se |
Aufsätze |
author-letter |
Ma, Bin |
doi_str_mv |
10.1007/s10040-016-1525-5 |
dewey-full |
550 |
title_sort |
evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes |
title_auth |
Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes |
abstract |
Abstract Subsurface-water flow pathways in three different land-use areas (non-irrigated grassland, poplar forest, and irrigated arable land) in the central North China Plain were investigated using oxygen (18O) and hydrogen (2H) isotopes in samples of precipitation, soils, and groundwater. Soil water in the top 10 cm was significantly affected by both evaporation and infiltration. Water at 10–40 cm depth in the grassland and arable land, and 10–60 cm in poplar forest, showed a relatively short residence time, as a substantial proportion of antecedent soil water was mixed with a 92-mm storm infiltration event, whereas below those depths (down to 150 cm), depleted $ δ^{18} $O spikes suggested that some storm water bypassed the shallow soil layers. Significant differences, in soil-water content and $ δ^{18} $O values, within a small area, suggested that the proportion of immobile soil water and water flowing in subsurface pathways varies depending on local vegetation cover, soil characteristics and irrigation applications. Soil-water $ δ^{18} $O values revealed that preferential flow and diffuse flow coexist. Preferential flow was active within the root zone, independent of antecedent soil-water content, in both poplar forest and arable land, whereas diffuse flow was observed in grassland. The depleted $ δ^{18} $O spikes at 20–50 cm depth in the arable land suggested the infiltration of irrigation water during the dry season. Temporal isotopic variations in precipitation were subdued in the shallow groundwater, suggesting more complete mixing of different input waters in the unsaturated zone before reaching the shallow groundwater. © Springer-Verlag Berlin Heidelberg 2017 |
abstractGer |
Abstract Subsurface-water flow pathways in three different land-use areas (non-irrigated grassland, poplar forest, and irrigated arable land) in the central North China Plain were investigated using oxygen (18O) and hydrogen (2H) isotopes in samples of precipitation, soils, and groundwater. Soil water in the top 10 cm was significantly affected by both evaporation and infiltration. Water at 10–40 cm depth in the grassland and arable land, and 10–60 cm in poplar forest, showed a relatively short residence time, as a substantial proportion of antecedent soil water was mixed with a 92-mm storm infiltration event, whereas below those depths (down to 150 cm), depleted $ δ^{18} $O spikes suggested that some storm water bypassed the shallow soil layers. Significant differences, in soil-water content and $ δ^{18} $O values, within a small area, suggested that the proportion of immobile soil water and water flowing in subsurface pathways varies depending on local vegetation cover, soil characteristics and irrigation applications. Soil-water $ δ^{18} $O values revealed that preferential flow and diffuse flow coexist. Preferential flow was active within the root zone, independent of antecedent soil-water content, in both poplar forest and arable land, whereas diffuse flow was observed in grassland. The depleted $ δ^{18} $O spikes at 20–50 cm depth in the arable land suggested the infiltration of irrigation water during the dry season. Temporal isotopic variations in precipitation were subdued in the shallow groundwater, suggesting more complete mixing of different input waters in the unsaturated zone before reaching the shallow groundwater. © Springer-Verlag Berlin Heidelberg 2017 |
abstract_unstemmed |
Abstract Subsurface-water flow pathways in three different land-use areas (non-irrigated grassland, poplar forest, and irrigated arable land) in the central North China Plain were investigated using oxygen (18O) and hydrogen (2H) isotopes in samples of precipitation, soils, and groundwater. Soil water in the top 10 cm was significantly affected by both evaporation and infiltration. Water at 10–40 cm depth in the grassland and arable land, and 10–60 cm in poplar forest, showed a relatively short residence time, as a substantial proportion of antecedent soil water was mixed with a 92-mm storm infiltration event, whereas below those depths (down to 150 cm), depleted $ δ^{18} $O spikes suggested that some storm water bypassed the shallow soil layers. Significant differences, in soil-water content and $ δ^{18} $O values, within a small area, suggested that the proportion of immobile soil water and water flowing in subsurface pathways varies depending on local vegetation cover, soil characteristics and irrigation applications. Soil-water $ δ^{18} $O values revealed that preferential flow and diffuse flow coexist. Preferential flow was active within the root zone, independent of antecedent soil-water content, in both poplar forest and arable land, whereas diffuse flow was observed in grassland. The depleted $ δ^{18} $O spikes at 20–50 cm depth in the arable land suggested the infiltration of irrigation water during the dry season. Temporal isotopic variations in precipitation were subdued in the shallow groundwater, suggesting more complete mixing of different input waters in the unsaturated zone before reaching the shallow groundwater. © Springer-Verlag Berlin Heidelberg 2017 |
collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 GBV_ILN_183 GBV_ILN_267 GBV_ILN_2018 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4277 |
container_issue |
3 |
title_short |
Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes |
url |
https://doi.org/10.1007/s10040-016-1525-5 |
remote_bool |
false |
author2 |
Liang, Xing Liu, Shaohua Jin, Menggui Nimmo, John R. Li, Jing |
author2Str |
Liang, Xing Liu, Shaohua Jin, Menggui Nimmo, John R. Li, Jing |
ppnlink |
18393735X |
mediatype_str_mv |
n |
isOA_txt |
false |
hochschulschrift_bool |
false |
doi_str |
10.1007/s10040-016-1525-5 |
up_date |
2024-07-04T01:01:17.056Z |
_version_ |
1803608262764920832 |
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">OLC2040028307</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230502161125.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">200819s2017 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s10040-016-1525-5</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2040028307</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s10040-016-1525-5-p</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="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Ma, Bin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Evaluation of diffuse and preferential flow pathways of infiltrated precipitation and irrigation using oxygen and hydrogen isotopes</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2017</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">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag Berlin Heidelberg 2017</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Subsurface-water flow pathways in three different land-use areas (non-irrigated grassland, poplar forest, and irrigated arable land) in the central North China Plain were investigated using oxygen (18O) and hydrogen (2H) isotopes in samples of precipitation, soils, and groundwater. Soil water in the top 10 cm was significantly affected by both evaporation and infiltration. Water at 10–40 cm depth in the grassland and arable land, and 10–60 cm in poplar forest, showed a relatively short residence time, as a substantial proportion of antecedent soil water was mixed with a 92-mm storm infiltration event, whereas below those depths (down to 150 cm), depleted $ δ^{18} $O spikes suggested that some storm water bypassed the shallow soil layers. Significant differences, in soil-water content and $ δ^{18} $O values, within a small area, suggested that the proportion of immobile soil water and water flowing in subsurface pathways varies depending on local vegetation cover, soil characteristics and irrigation applications. Soil-water $ δ^{18} $O values revealed that preferential flow and diffuse flow coexist. Preferential flow was active within the root zone, independent of antecedent soil-water content, in both poplar forest and arable land, whereas diffuse flow was observed in grassland. The depleted $ δ^{18} $O spikes at 20–50 cm depth in the arable land suggested the infiltration of irrigation water during the dry season. Temporal isotopic variations in precipitation were subdued in the shallow groundwater, suggesting more complete mixing of different input waters in the unsaturated zone before reaching the shallow groundwater.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Stable isotopes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Unsaturated zone</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Diffuse flow</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Preferential flow</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">China</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liang, Xing</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liu, Shaohua</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Jin, Menggui</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Nimmo, John R.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Li, Jing</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Hydrogeology journal</subfield><subfield code="d">Springer Berlin Heidelberg, 1995</subfield><subfield code="g">25(2017), 3 vom: 07. Jan., Seite 675-688</subfield><subfield code="w">(DE-627)18393735X</subfield><subfield code="w">(DE-600)1227482-3</subfield><subfield code="w">(DE-576)045314829</subfield><subfield code="x">1431-2174</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:25</subfield><subfield code="g">year:2017</subfield><subfield code="g">number:3</subfield><subfield code="g">day:07</subfield><subfield code="g">month:01</subfield><subfield code="g">pages:675-688</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s10040-016-1525-5</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</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_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</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_183</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_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4046</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_4277</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">25</subfield><subfield code="j">2017</subfield><subfield code="e">3</subfield><subfield code="b">07</subfield><subfield code="c">01</subfield><subfield code="h">675-688</subfield></datafield></record></collection>
|
score |
7.400462 |