Interrill soil erosion processes on steep slopes
• Rainfall intensity affects both soil detachment and sediment transport. • Sediment transport process controls sheet erosion rate. • Sediment transport modes vary with flow depth and slope length. • Optimal mean flow depth for maximal sheet erosion rate was less than 0.1mm. • Slope length was negat...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Zhang, X.C. John [verfasserIn] |
|---|
| Format: |
E-Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2017 |
|---|
| Schlagwörter: |
|---|
| Umfang: |
13 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China - Liu, Huiying ELSEVIER, 2021, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:548 ; year:2017 ; pages:652-664 ; extent:13 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.jhydrol.2017.03.046 |
|---|
| Katalog-ID: |
ELV025650297 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | ELV025650297 | ||
| 003 | DE-627 | ||
| 005 | 20230623181357.0 | ||
| 007 | cr uuu---uuuuu | ||
| 008 | 180603s2017 xx |||||o 00| ||eng c | ||
| 024 | 7 | |a 10.1016/j.jhydrol.2017.03.046 |2 doi | |
| 028 | 5 | 2 | |a GBV00000000000092A.pica |
| 035 | |a (DE-627)ELV025650297 | ||
| 035 | |a (ELSEVIER)S0022-1694(17)30192-0 | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | |a 690 | |
| 082 | 0 | 4 | |a 690 |q DE-600 |
| 082 | 0 | 4 | |a 610 |q VZ |
| 084 | |a 74.00 |2 bkl | ||
| 084 | |a 44.73 |2 bkl | ||
| 100 | 1 | |a Zhang, X.C. John |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Interrill soil erosion processes on steep slopes |
| 264 | 1 | |c 2017 | |
| 300 | |a 13 | ||
| 336 | |a nicht spezifiziert |b zzz |2 rdacontent | ||
| 337 | |a nicht spezifiziert |b z |2 rdamedia | ||
| 338 | |a nicht spezifiziert |b zu |2 rdacarrier | ||
| 520 | |a • Rainfall intensity affects both soil detachment and sediment transport. • Sediment transport process controls sheet erosion rate. • Sediment transport modes vary with flow depth and slope length. • Optimal mean flow depth for maximal sheet erosion rate was less than 0.1mm. • Slope length was negatively related to sheet erosion rate per unit area. | ||
| 650 | 7 | |a Interrill erosion modeling |2 Elsevier | |
| 650 | 7 | |a Soil detachment |2 Elsevier | |
| 650 | 7 | |a Interrill erosion process |2 Elsevier | |
| 650 | 7 | |a Sediment transport |2 Elsevier | |
| 700 | 1 | |a Wang, Z.L. |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier |a Liu, Huiying ELSEVIER |t Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China |d 2021 |g Amsterdam [u.a.] |w (DE-627)ELV007566492 |
| 773 | 1 | 8 | |g volume:548 |g year:2017 |g pages:652-664 |g extent:13 |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.jhydrol.2017.03.046 |3 Volltext |
| 912 | |a GBV_USEFLAG_U | ||
| 912 | |a GBV_ELV | ||
| 912 | |a SYSFLAG_U | ||
| 912 | |a SSG-OLC-PHA | ||
| 912 | |a SSG-OPC-GGO | ||
| 936 | b | k | |a 74.00 |j Geographie |j Anthropogeographie: Allgemeines |q VZ |
| 936 | b | k | |a 44.73 |j Geomedizin |q VZ |
| 951 | |a AR | ||
| 952 | |d 548 |j 2017 |h 652-664 |g 13 | ||
| 953 | |2 045F |a 690 | ||
| author_variant |
x j z xj xjz |
|---|---|
| matchkey_str |
zhangxcjohnwangzl:2017----:nerlsieoinrcseo |
| hierarchy_sort_str |
2017 |
| bklnumber |
74.00 44.73 |
| publishDate |
2017 |
| allfields |
10.1016/j.jhydrol.2017.03.046 doi GBV00000000000092A.pica (DE-627)ELV025650297 (ELSEVIER)S0022-1694(17)30192-0 DE-627 ger DE-627 rakwb eng 690 690 DE-600 610 VZ 74.00 bkl 44.73 bkl Zhang, X.C. John verfasserin aut Interrill soil erosion processes on steep slopes 2017 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • Rainfall intensity affects both soil detachment and sediment transport. • Sediment transport process controls sheet erosion rate. • Sediment transport modes vary with flow depth and slope length. • Optimal mean flow depth for maximal sheet erosion rate was less than 0.1mm. • Slope length was negatively related to sheet erosion rate per unit area. Interrill erosion modeling Elsevier Soil detachment Elsevier Interrill erosion process Elsevier Sediment transport Elsevier Wang, Z.L. oth Enthalten in Elsevier Liu, Huiying ELSEVIER Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China 2021 Amsterdam [u.a.] (DE-627)ELV007566492 volume:548 year:2017 pages:652-664 extent:13 https://doi.org/10.1016/j.jhydrol.2017.03.046 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA SSG-OPC-GGO 74.00 Geographie Anthropogeographie: Allgemeines VZ 44.73 Geomedizin VZ AR 548 2017 652-664 13 045F 690 |
| spelling |
10.1016/j.jhydrol.2017.03.046 doi GBV00000000000092A.pica (DE-627)ELV025650297 (ELSEVIER)S0022-1694(17)30192-0 DE-627 ger DE-627 rakwb eng 690 690 DE-600 610 VZ 74.00 bkl 44.73 bkl Zhang, X.C. John verfasserin aut Interrill soil erosion processes on steep slopes 2017 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • Rainfall intensity affects both soil detachment and sediment transport. • Sediment transport process controls sheet erosion rate. • Sediment transport modes vary with flow depth and slope length. • Optimal mean flow depth for maximal sheet erosion rate was less than 0.1mm. • Slope length was negatively related to sheet erosion rate per unit area. Interrill erosion modeling Elsevier Soil detachment Elsevier Interrill erosion process Elsevier Sediment transport Elsevier Wang, Z.L. oth Enthalten in Elsevier Liu, Huiying ELSEVIER Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China 2021 Amsterdam [u.a.] (DE-627)ELV007566492 volume:548 year:2017 pages:652-664 extent:13 https://doi.org/10.1016/j.jhydrol.2017.03.046 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA SSG-OPC-GGO 74.00 Geographie Anthropogeographie: Allgemeines VZ 44.73 Geomedizin VZ AR 548 2017 652-664 13 045F 690 |
| allfields_unstemmed |
10.1016/j.jhydrol.2017.03.046 doi GBV00000000000092A.pica (DE-627)ELV025650297 (ELSEVIER)S0022-1694(17)30192-0 DE-627 ger DE-627 rakwb eng 690 690 DE-600 610 VZ 74.00 bkl 44.73 bkl Zhang, X.C. John verfasserin aut Interrill soil erosion processes on steep slopes 2017 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • Rainfall intensity affects both soil detachment and sediment transport. • Sediment transport process controls sheet erosion rate. • Sediment transport modes vary with flow depth and slope length. • Optimal mean flow depth for maximal sheet erosion rate was less than 0.1mm. • Slope length was negatively related to sheet erosion rate per unit area. Interrill erosion modeling Elsevier Soil detachment Elsevier Interrill erosion process Elsevier Sediment transport Elsevier Wang, Z.L. oth Enthalten in Elsevier Liu, Huiying ELSEVIER Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China 2021 Amsterdam [u.a.] (DE-627)ELV007566492 volume:548 year:2017 pages:652-664 extent:13 https://doi.org/10.1016/j.jhydrol.2017.03.046 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA SSG-OPC-GGO 74.00 Geographie Anthropogeographie: Allgemeines VZ 44.73 Geomedizin VZ AR 548 2017 652-664 13 045F 690 |
| allfieldsGer |
10.1016/j.jhydrol.2017.03.046 doi GBV00000000000092A.pica (DE-627)ELV025650297 (ELSEVIER)S0022-1694(17)30192-0 DE-627 ger DE-627 rakwb eng 690 690 DE-600 610 VZ 74.00 bkl 44.73 bkl Zhang, X.C. John verfasserin aut Interrill soil erosion processes on steep slopes 2017 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • Rainfall intensity affects both soil detachment and sediment transport. • Sediment transport process controls sheet erosion rate. • Sediment transport modes vary with flow depth and slope length. • Optimal mean flow depth for maximal sheet erosion rate was less than 0.1mm. • Slope length was negatively related to sheet erosion rate per unit area. Interrill erosion modeling Elsevier Soil detachment Elsevier Interrill erosion process Elsevier Sediment transport Elsevier Wang, Z.L. oth Enthalten in Elsevier Liu, Huiying ELSEVIER Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China 2021 Amsterdam [u.a.] (DE-627)ELV007566492 volume:548 year:2017 pages:652-664 extent:13 https://doi.org/10.1016/j.jhydrol.2017.03.046 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA SSG-OPC-GGO 74.00 Geographie Anthropogeographie: Allgemeines VZ 44.73 Geomedizin VZ AR 548 2017 652-664 13 045F 690 |
| allfieldsSound |
10.1016/j.jhydrol.2017.03.046 doi GBV00000000000092A.pica (DE-627)ELV025650297 (ELSEVIER)S0022-1694(17)30192-0 DE-627 ger DE-627 rakwb eng 690 690 DE-600 610 VZ 74.00 bkl 44.73 bkl Zhang, X.C. John verfasserin aut Interrill soil erosion processes on steep slopes 2017 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier • Rainfall intensity affects both soil detachment and sediment transport. • Sediment transport process controls sheet erosion rate. • Sediment transport modes vary with flow depth and slope length. • Optimal mean flow depth for maximal sheet erosion rate was less than 0.1mm. • Slope length was negatively related to sheet erosion rate per unit area. Interrill erosion modeling Elsevier Soil detachment Elsevier Interrill erosion process Elsevier Sediment transport Elsevier Wang, Z.L. oth Enthalten in Elsevier Liu, Huiying ELSEVIER Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China 2021 Amsterdam [u.a.] (DE-627)ELV007566492 volume:548 year:2017 pages:652-664 extent:13 https://doi.org/10.1016/j.jhydrol.2017.03.046 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA SSG-OPC-GGO 74.00 Geographie Anthropogeographie: Allgemeines VZ 44.73 Geomedizin VZ AR 548 2017 652-664 13 045F 690 |
| language |
English |
| source |
Enthalten in Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China Amsterdam [u.a.] volume:548 year:2017 pages:652-664 extent:13 |
| sourceStr |
Enthalten in Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China Amsterdam [u.a.] volume:548 year:2017 pages:652-664 extent:13 |
| format_phy_str_mv |
Article |
| bklname |
Geographie Anthropogeographie: Allgemeines Geomedizin |
| institution |
findex.gbv.de |
| topic_facet |
Interrill erosion modeling Soil detachment Interrill erosion process Sediment transport |
| dewey-raw |
690 |
| isfreeaccess_bool |
false |
| container_title |
Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China |
| authorswithroles_txt_mv |
Zhang, X.C. John @@aut@@ Wang, Z.L. @@oth@@ |
| publishDateDaySort_date |
2017-01-01T00:00:00Z |
| hierarchy_top_id |
ELV007566492 |
| dewey-sort |
3690 |
| id |
ELV025650297 |
| 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">ELV025650297</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230623181357.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">180603s2017 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.jhydrol.2017.03.046</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">GBV00000000000092A.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV025650297</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0022-1694(17)30192-0</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=" "><subfield code="a">690</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">690</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">610</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">74.00</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">44.73</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhang, X.C. John</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Interrill soil erosion processes on steep slopes</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2017</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">13</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">• Rainfall intensity affects both soil detachment and sediment transport. • Sediment transport process controls sheet erosion rate. • Sediment transport modes vary with flow depth and slope length. • Optimal mean flow depth for maximal sheet erosion rate was less than 0.1mm. • Slope length was negatively related to sheet erosion rate per unit area.</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Interrill erosion modeling</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Soil detachment</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Interrill erosion process</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Sediment transport</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wang, Z.L.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier</subfield><subfield code="a">Liu, Huiying ELSEVIER</subfield><subfield code="t">Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China</subfield><subfield code="d">2021</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV007566492</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:548</subfield><subfield code="g">year:2017</subfield><subfield code="g">pages:652-664</subfield><subfield code="g">extent:13</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.jhydrol.2017.03.046</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">74.00</subfield><subfield code="j">Geographie</subfield><subfield code="j">Anthropogeographie: Allgemeines</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">44.73</subfield><subfield code="j">Geomedizin</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">548</subfield><subfield code="j">2017</subfield><subfield code="h">652-664</subfield><subfield code="g">13</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">690</subfield></datafield></record></collection>
|
| author |
Zhang, X.C. John |
| spellingShingle |
Zhang, X.C. John ddc 690 ddc 610 bkl 74.00 bkl 44.73 Elsevier Interrill erosion modeling Elsevier Soil detachment Elsevier Interrill erosion process Elsevier Sediment transport Interrill soil erosion processes on steep slopes |
| authorStr |
Zhang, X.C. John |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)ELV007566492 |
| format |
electronic Article |
| dewey-ones |
690 - Buildings 610 - Medicine & health |
| delete_txt_mv |
keep |
| author_role |
aut |
| collection |
elsevier |
| remote_str |
true |
| illustrated |
Not Illustrated |
| topic_title |
690 690 DE-600 610 VZ 74.00 bkl 44.73 bkl Interrill soil erosion processes on steep slopes Interrill erosion modeling Elsevier Soil detachment Elsevier Interrill erosion process Elsevier Sediment transport Elsevier |
| topic |
ddc 690 ddc 610 bkl 74.00 bkl 44.73 Elsevier Interrill erosion modeling Elsevier Soil detachment Elsevier Interrill erosion process Elsevier Sediment transport |
| topic_unstemmed |
ddc 690 ddc 610 bkl 74.00 bkl 44.73 Elsevier Interrill erosion modeling Elsevier Soil detachment Elsevier Interrill erosion process Elsevier Sediment transport |
| topic_browse |
ddc 690 ddc 610 bkl 74.00 bkl 44.73 Elsevier Interrill erosion modeling Elsevier Soil detachment Elsevier Interrill erosion process Elsevier Sediment transport |
| format_facet |
Elektronische Aufsätze Aufsätze Elektronische Ressource |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
zu |
| author2_variant |
z w zw |
| hierarchy_parent_title |
Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China |
| hierarchy_parent_id |
ELV007566492 |
| dewey-tens |
690 - Building & construction 610 - Medicine & health |
| hierarchy_top_title |
Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)ELV007566492 |
| title |
Interrill soil erosion processes on steep slopes |
| ctrlnum |
(DE-627)ELV025650297 (ELSEVIER)S0022-1694(17)30192-0 |
| title_full |
Interrill soil erosion processes on steep slopes |
| author_sort |
Zhang, X.C. John |
| journal |
Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China |
| journalStr |
Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
600 - Technology |
| recordtype |
marc |
| publishDateSort |
2017 |
| contenttype_str_mv |
zzz |
| container_start_page |
652 |
| author_browse |
Zhang, X.C. John |
| container_volume |
548 |
| physical |
13 |
| class |
690 690 DE-600 610 VZ 74.00 bkl 44.73 bkl |
| format_se |
Elektronische Aufsätze |
| author-letter |
Zhang, X.C. John |
| doi_str_mv |
10.1016/j.jhydrol.2017.03.046 |
| dewey-full |
690 610 |
| title_sort |
interrill soil erosion processes on steep slopes |
| title_auth |
Interrill soil erosion processes on steep slopes |
| abstract |
• Rainfall intensity affects both soil detachment and sediment transport. • Sediment transport process controls sheet erosion rate. • Sediment transport modes vary with flow depth and slope length. • Optimal mean flow depth for maximal sheet erosion rate was less than 0.1mm. • Slope length was negatively related to sheet erosion rate per unit area. |
| abstractGer |
• Rainfall intensity affects both soil detachment and sediment transport. • Sediment transport process controls sheet erosion rate. • Sediment transport modes vary with flow depth and slope length. • Optimal mean flow depth for maximal sheet erosion rate was less than 0.1mm. • Slope length was negatively related to sheet erosion rate per unit area. |
| abstract_unstemmed |
• Rainfall intensity affects both soil detachment and sediment transport. • Sediment transport process controls sheet erosion rate. • Sediment transport modes vary with flow depth and slope length. • Optimal mean flow depth for maximal sheet erosion rate was less than 0.1mm. • Slope length was negatively related to sheet erosion rate per unit area. |
| collection_details |
GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA SSG-OPC-GGO |
| title_short |
Interrill soil erosion processes on steep slopes |
| url |
https://doi.org/10.1016/j.jhydrol.2017.03.046 |
| remote_bool |
true |
| author2 |
Wang, Z.L. |
| author2Str |
Wang, Z.L. |
| ppnlink |
ELV007566492 |
| mediatype_str_mv |
z |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| author2_role |
oth |
| doi_str |
10.1016/j.jhydrol.2017.03.046 |
| up_date |
2024-07-06T18:06:23.696Z |
| _version_ |
1803853951084265472 |
| 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">ELV025650297</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230623181357.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">180603s2017 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.jhydrol.2017.03.046</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">GBV00000000000092A.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV025650297</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0022-1694(17)30192-0</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=" "><subfield code="a">690</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">690</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">610</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">74.00</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">44.73</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhang, X.C. John</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Interrill soil erosion processes on steep slopes</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2017</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">13</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">z</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zu</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">• Rainfall intensity affects both soil detachment and sediment transport. • Sediment transport process controls sheet erosion rate. • Sediment transport modes vary with flow depth and slope length. • Optimal mean flow depth for maximal sheet erosion rate was less than 0.1mm. • Slope length was negatively related to sheet erosion rate per unit area.</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Interrill erosion modeling</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Soil detachment</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Interrill erosion process</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="650" ind1=" " ind2="7"><subfield code="a">Sediment transport</subfield><subfield code="2">Elsevier</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wang, Z.L.</subfield><subfield code="4">oth</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="n">Elsevier</subfield><subfield code="a">Liu, Huiying ELSEVIER</subfield><subfield code="t">Neighborhood resources associated with frailty trajectories over time among community-dwelling older adults in China</subfield><subfield code="d">2021</subfield><subfield code="g">Amsterdam [u.a.]</subfield><subfield code="w">(DE-627)ELV007566492</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:548</subfield><subfield code="g">year:2017</subfield><subfield code="g">pages:652-664</subfield><subfield code="g">extent:13</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.jhydrol.2017.03.046</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">74.00</subfield><subfield code="j">Geographie</subfield><subfield code="j">Anthropogeographie: Allgemeines</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">44.73</subfield><subfield code="j">Geomedizin</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">548</subfield><subfield code="j">2017</subfield><subfield code="h">652-664</subfield><subfield code="g">13</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">690</subfield></datafield></record></collection>
|
| score |
7.402815 |