Soil geochemistry of medieval arable fields in Lovětín near Třešť, Czech Republic
Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Horák, Jan [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2018transfer abstract |
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| Umfang: |
9 |
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| Übergeordnetes Werk: |
Enthalten in: Towards unravelling the Rosette agent enigma: Spread and emergence of the co-invasive host-pathogen complex, - Marine, Combe ELSEVIER, 2021, an interdisciplinary journal of soil science, hydrology, geomorphology focusing on geoecology and landscape evolution, New York, NY [u.a.] |
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| Übergeordnetes Werk: |
volume:162 ; year:2018 ; pages:14-22 ; extent:9 |
| Links: |
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| DOI / URN: |
10.1016/j.catena.2017.11.014 |
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| Katalog-ID: |
ELV041440684 |
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| 245 | 1 | 0 | |a Soil geochemistry of medieval arable fields in Lovětín near Třešť, Czech Republic |
| 264 | 1 | |c 2018transfer abstract | |
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| 520 | |a Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies. | ||
| 520 | |a Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies. | ||
| 700 | 1 | |a Janovský, Martin |4 oth | |
| 700 | 1 | |a Hejcman, Michal |4 oth | |
| 700 | 1 | |a Šmejda, Ladislav |4 oth | |
| 700 | 1 | |a Klír, Tomáš |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier |a Marine, Combe ELSEVIER |t Towards unravelling the Rosette agent enigma: Spread and emergence of the co-invasive host-pathogen complex, |d 2021 |d an interdisciplinary journal of soil science, hydrology, geomorphology focusing on geoecology and landscape evolution |g New York, NY [u.a.] |w (DE-627)ELV006991912 |
| 773 | 1 | 8 | |g volume:162 |g year:2018 |g pages:14-22 |g extent:9 |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.catena.2017.11.014 |3 Volltext |
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10.1016/j.catena.2017.11.014 doi GBV00000000000193A.pica (DE-627)ELV041440684 (ELSEVIER)S0341-8162(17)30382-X DE-627 ger DE-627 rakwb eng 910 550 910 DE-600 550 DE-600 333.7 610 VZ 43.12 bkl 43.13 bkl 44.13 bkl Horák, Jan verfasserin aut Soil geochemistry of medieval arable fields in Lovětín near Třešť, Czech Republic 2018transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies. Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies. Janovský, Martin oth Hejcman, Michal oth Šmejda, Ladislav oth Klír, Tomáš oth Enthalten in Elsevier Marine, Combe ELSEVIER Towards unravelling the Rosette agent enigma: Spread and emergence of the co-invasive host-pathogen complex, 2021 an interdisciplinary journal of soil science, hydrology, geomorphology focusing on geoecology and landscape evolution New York, NY [u.a.] (DE-627)ELV006991912 volume:162 year:2018 pages:14-22 extent:9 https://doi.org/10.1016/j.catena.2017.11.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA SSG-OPC-GGO 43.12 Umweltchemie VZ 43.13 Umwelttoxikologie VZ 44.13 Medizinische Ökologie VZ AR 162 2018 14-22 9 045F 910 |
| spelling |
10.1016/j.catena.2017.11.014 doi GBV00000000000193A.pica (DE-627)ELV041440684 (ELSEVIER)S0341-8162(17)30382-X DE-627 ger DE-627 rakwb eng 910 550 910 DE-600 550 DE-600 333.7 610 VZ 43.12 bkl 43.13 bkl 44.13 bkl Horák, Jan verfasserin aut Soil geochemistry of medieval arable fields in Lovětín near Třešť, Czech Republic 2018transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies. Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies. Janovský, Martin oth Hejcman, Michal oth Šmejda, Ladislav oth Klír, Tomáš oth Enthalten in Elsevier Marine, Combe ELSEVIER Towards unravelling the Rosette agent enigma: Spread and emergence of the co-invasive host-pathogen complex, 2021 an interdisciplinary journal of soil science, hydrology, geomorphology focusing on geoecology and landscape evolution New York, NY [u.a.] (DE-627)ELV006991912 volume:162 year:2018 pages:14-22 extent:9 https://doi.org/10.1016/j.catena.2017.11.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA SSG-OPC-GGO 43.12 Umweltchemie VZ 43.13 Umwelttoxikologie VZ 44.13 Medizinische Ökologie VZ AR 162 2018 14-22 9 045F 910 |
| allfields_unstemmed |
10.1016/j.catena.2017.11.014 doi GBV00000000000193A.pica (DE-627)ELV041440684 (ELSEVIER)S0341-8162(17)30382-X DE-627 ger DE-627 rakwb eng 910 550 910 DE-600 550 DE-600 333.7 610 VZ 43.12 bkl 43.13 bkl 44.13 bkl Horák, Jan verfasserin aut Soil geochemistry of medieval arable fields in Lovětín near Třešť, Czech Republic 2018transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies. Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies. Janovský, Martin oth Hejcman, Michal oth Šmejda, Ladislav oth Klír, Tomáš oth Enthalten in Elsevier Marine, Combe ELSEVIER Towards unravelling the Rosette agent enigma: Spread and emergence of the co-invasive host-pathogen complex, 2021 an interdisciplinary journal of soil science, hydrology, geomorphology focusing on geoecology and landscape evolution New York, NY [u.a.] (DE-627)ELV006991912 volume:162 year:2018 pages:14-22 extent:9 https://doi.org/10.1016/j.catena.2017.11.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA SSG-OPC-GGO 43.12 Umweltchemie VZ 43.13 Umwelttoxikologie VZ 44.13 Medizinische Ökologie VZ AR 162 2018 14-22 9 045F 910 |
| allfieldsGer |
10.1016/j.catena.2017.11.014 doi GBV00000000000193A.pica (DE-627)ELV041440684 (ELSEVIER)S0341-8162(17)30382-X DE-627 ger DE-627 rakwb eng 910 550 910 DE-600 550 DE-600 333.7 610 VZ 43.12 bkl 43.13 bkl 44.13 bkl Horák, Jan verfasserin aut Soil geochemistry of medieval arable fields in Lovětín near Třešť, Czech Republic 2018transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies. Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies. Janovský, Martin oth Hejcman, Michal oth Šmejda, Ladislav oth Klír, Tomáš oth Enthalten in Elsevier Marine, Combe ELSEVIER Towards unravelling the Rosette agent enigma: Spread and emergence of the co-invasive host-pathogen complex, 2021 an interdisciplinary journal of soil science, hydrology, geomorphology focusing on geoecology and landscape evolution New York, NY [u.a.] (DE-627)ELV006991912 volume:162 year:2018 pages:14-22 extent:9 https://doi.org/10.1016/j.catena.2017.11.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA SSG-OPC-GGO 43.12 Umweltchemie VZ 43.13 Umwelttoxikologie VZ 44.13 Medizinische Ökologie VZ AR 162 2018 14-22 9 045F 910 |
| allfieldsSound |
10.1016/j.catena.2017.11.014 doi GBV00000000000193A.pica (DE-627)ELV041440684 (ELSEVIER)S0341-8162(17)30382-X DE-627 ger DE-627 rakwb eng 910 550 910 DE-600 550 DE-600 333.7 610 VZ 43.12 bkl 43.13 bkl 44.13 bkl Horák, Jan verfasserin aut Soil geochemistry of medieval arable fields in Lovětín near Třešť, Czech Republic 2018transfer abstract 9 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies. Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies. Janovský, Martin oth Hejcman, Michal oth Šmejda, Ladislav oth Klír, Tomáš oth Enthalten in Elsevier Marine, Combe ELSEVIER Towards unravelling the Rosette agent enigma: Spread and emergence of the co-invasive host-pathogen complex, 2021 an interdisciplinary journal of soil science, hydrology, geomorphology focusing on geoecology and landscape evolution New York, NY [u.a.] (DE-627)ELV006991912 volume:162 year:2018 pages:14-22 extent:9 https://doi.org/10.1016/j.catena.2017.11.014 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U SSG-OLC-PHA SSG-OPC-GGO 43.12 Umweltchemie VZ 43.13 Umwelttoxikologie VZ 44.13 Medizinische Ökologie VZ AR 162 2018 14-22 9 045F 910 |
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Soil geochemistry of medieval arable fields in Lovětín near Třešť, Czech Republic |
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Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies. |
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Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies. |
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Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies. |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV041440684</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230625234615.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">180726s2018 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.catena.2017.11.014</subfield><subfield code="2">doi</subfield></datafield><datafield tag="028" ind1="5" ind2="2"><subfield code="a">GBV00000000000193A.pica</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV041440684</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0341-8162(17)30382-X</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">910</subfield><subfield code="a">550</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">910</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">333.7</subfield><subfield code="a">610</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">43.12</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">43.13</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">44.13</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Horák, Jan</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Soil geochemistry of medieval arable fields in Lovětín near Třešť, Czech Republic</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2018transfer abstract</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">9</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">Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Lovětín was a medieval village located in the Bohemian-Moravian Upland (Czech Republic). It existed approximately between the 14th and the 16th century and was comprised of up to 20 farmsteads. Arable farming based on a short-fallow cultivation system was its main means of subsistence. The fields of the village consisted of two main field areas (128 and 77ha) and six smaller field areas (up to 8ha). Our study focused on finding out how human activities have impacted the soil environment imprinted in its geochemical characteristics. The design was based on a 100-m grid (in some cases, a 50-m grid) covering the entire field system (plužina) of the village; soil samples were taken from the B horizon at a depth of 15cm. The analysis was based on XRF spectrometry, returning near total concentrations of the elements. The statistical and GIS analyses were performed on 338 samples, measuring the following elements: Al, Si, K, Ti, Cr, Mn, Fe, Ni, Cu, Zn, As, Rb, Sr, Zr, Pb, Th, LE (light elements – combined concentrations for H to Na). The results of the analyses were processed by PCA after ilr transformation. The PCA indicated 16 principal components, of which three were interpreted as direct products of past human activities. The main elements reflecting human activities were Mn, Sr, Th, K, Zn; P contributed also to the interpretations, although it was detected and measured only in 132 cases. Some of the elements were spatially connected to the village in terms of their concentrations, but the PCA did not reveal a strong connection (Ti, Cr, Ni, Cu, Zr). The spatial distribution of the principal components was varied, indicating a diversity in the spatial distribution of agricultural activities or of their intensity, as well as differences in land use management. Management was most intensive in the vicinity of the village built-up area up to a distance of 300–400m. The village was probably deserted due to inadequate soil management strategies.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Janovský, Martin</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Hejcman, Michal</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Šmejda, Ladislav</subfield><subfield code="4">oth</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Klír, Tomáš</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">Marine, Combe ELSEVIER</subfield><subfield code="t">Towards unravelling the Rosette agent enigma: Spread and emergence of the co-invasive host-pathogen complex,</subfield><subfield code="d">2021</subfield><subfield code="d">an interdisciplinary journal of soil science, hydrology, geomorphology focusing on geoecology and landscape evolution</subfield><subfield code="g">New York, NY [u.a.]</subfield><subfield code="w">(DE-627)ELV006991912</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:162</subfield><subfield code="g">year:2018</subfield><subfield code="g">pages:14-22</subfield><subfield code="g">extent:9</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1016/j.catena.2017.11.014</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">43.12</subfield><subfield code="j">Umweltchemie</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">43.13</subfield><subfield code="j">Umwelttoxikologie</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">44.13</subfield><subfield code="j">Medizinische Ökologie</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">162</subfield><subfield code="j">2018</subfield><subfield code="h">14-22</subfield><subfield code="g">9</subfield></datafield><datafield tag="953" ind1=" " ind2=" "><subfield code="2">045F</subfield><subfield code="a">910</subfield></datafield></record></collection>
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