AB

Bibliografia publikacji pracowników
Państwowej Szkoły Wyższej w Białej Podlaskiej

Baza tworzona przez Bibliotekę Akademii Bialskiej im. Jana Pawła II.


Zapytanie: ROGÓŻ-MATYSZCZAK ANNA
Liczba odnalezionych rekordów: 10



Przejście do opcji zmiany formatu | Wyświetl/ukryj etykiety | Wyświetlenie wyników w wersji do druku | Pobranie pliku do edytora | Nowe wyszukiwanie
1/10
Nr opisu: f2928979007^aEnvironmental Change Documented in the Fluvial Landscape^ba Case sTudy of the Late Neolithic Bršadin-Pašnjak Pod Delom Site (NE Croatia)^aEnvironmental Archeology^kThe Journal of Human Palaeoecology^a2024^aOnline first.^a1749-6314^a2024/2025^a10.1080/14614103.2024.2408182^aNitychoruk, Jerzy^cx^ax^a5th millennium cal BC^aThe formation of Neolithic tell settlements in wetlands or near watercourses is documented in the published literature, but their research is not often based on environmental study. In this paper, we present the results from two sediment cores (BR1, BR2) collected from the case study archaeological site, located on the former bank of one of the Danube's tributaries in the southern Carpathian Basin. Although it has been suggested that a waterlogged environment was deliberately selected for this type of settlement in the regional Late Neolithic, the results of this study, based on both archaeological and environmental data, indicate dry and cool conditions prior and during the initial phase of the settlement formation. The abandonment of the settlement, possibly in the late 5th millennium, probably occurred due to alternating dry and wet episodes, rather than a gradual increase in wet conditions, as suggested elsewhere in the region. A large ditch encircling the settlement, not documented by archaeological research, can be indirectly confirmed by the BR2 core results and the analysis of aerial and satellite images. In general, there is a good correlation of results with the major global climate events, but there are differences in regional and wider south-eastern European context.^aarcheological record^aenvironmental change^afreshwater fauna^asoil chemistry^asouthern Carpathian Basin
Autorzy: , .
Tytuł pracy w innym języku: CzajkowskaCabała997700009997.800003Environmental Change Documented in the Fluvial LandscapeEnvironmental Archeology2024Online first.1749-63142024/202510.1080/14614103.2024.2408182Nitychoruk, Jerzyx5th millennium cal BCThe formation of Neolithic tell settlements in wetlands or near watercourses is documented in the published literature, but their research is not often based on environmental study. In this paper, we present the results from two sediment cores (BR1, BR2) collected from the case study archaeological site, located on the former bank of one of the Danube's tributaries in the southern Carpathian Basin. Although it has been suggested that a waterlogged environment was deliberately selected for this type of settlement in the regional Late Neolithic, the results of this study, based on both archaeological and environmental data, indicate dry and cool conditions prior and during the initial phase of the settlement formation. The abandonment of the settlement, possibly in the late 5th millennium, probably occurred due to alternating dry and wet episodes, rather than a gradual increase in wet conditions, as suggested elsewhere in the region. A large ditch encircling the settlement, not documented by archaeological research, can be indirectly confirmed by the BR2 core results and the analysis of aerial and satellite images. In general, there is a good correlation of results with the major global climate events, but there are differences in regional and wider south-eastern European context.archeological recordenvironmental changefreshwater faunasoil chemistrysouthern Carpathian Basin : Monika : Izabela : 999999LISTA FILADELFIJSKAIMPACT FACTOR : 009999.000 : Z : 003 : a Case sTudy of the Late Neolithic Bršadin-Pašnjak Pod Delom Site (NE Croatia)
Tytuł czasopisma:
Strony: CzajkowskaCabała997700009997.800003Environmental Change Documented in the Fluvial LandscapeEnvironmental Archeology2024Online first.1749-63142024/202510.1080/14614103.2024.2408182Nitychoruk, Jerzyx5th millennium cal BCThe formation of Neolithic tell settlements in wetlands or near watercourses is documented in the published literature, but their research is not often based on environmental study. In this paper, we present the results from two sediment cores (BR1, BR2) collected from the case study archaeological site, located on the former bank of one of the Danube's tributaries in the southern Carpathian Basin. Although it has been suggested that a waterlogged environment was deliberately selected for this type of settlement in the regional Late Neolithic, the results of this study, based on both archaeological and environmental data, indicate dry and cool conditions prior and during the initial phase of the settlement formation. The abandonment of the settlement, possibly in the late 5th millennium, probably occurred due to alternating dry and wet episodes, rather than a gradual increase in wet conditions, as suggested elsewhere in the region. A large ditch encircling the settlement, not documented by archaeological research, can be indirectly confirmed by the BR2 core results and the analysis of aerial and satellite images. In general, there is a good correlation of results with the major global climate event, Monika, Izabela, 999999LISTA FILADELFIJSKAIMPACT FACTOR, 009999.000, Z, 003, a Case sTudy of the Late Neolithic Bršadin-Pašnjak Pod Delom Site (NE Croatia), , , 009999.000, 2025-02-07, 12:31, x, , , 009999.000202420242024Environmental Change Documented in the Fluvial Landscape a Case sTudy of the Late Neolithic Bršad00000486160000000072AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttps://www.tandfonline.com/doi/full/10.1080/14614103.2024.2408182100, 2025-02-07, 12:32
Miejsce wydania: CzajkowskaCabała : Monika,
Charakterystyka merytoryczna:
Język publikacji:
Wskaźnik Impact Factor ISI:
Praca recenzowana
Słowa kluczowe: 79007^aEnvironmental Change Documented in the Fluvial Landscape^ba Case sTudy of the Late Neolithic Bršadin-Pašnjak Pod Delom Site (NE Croatia)^aEnvironmental Archeology^kThe Journal of Human Palaeoecology^a2024^aOnline first.^a1749-6314^a2024/2025^a10.1080/14614103.2024.2408182^aNitychoruk, Jerzy^cx^ax^a5th millennium cal BC^aThe formation of Neolithic tell settlements in wetlands or near watercourses is documented in the published literature, but their research is not often based on environmental study. In this paper, we present the results from two sediment cores (BR1, BR2) collected from the case study archaeological site, located on the former bank of one of the Danube's tributaries in the southern Carpathian Basin. Although it has been suggested that a waterlogged environment was deliberately selected for this type of settlement in the regional Late Neolithic, the results of this study, based on both archaeological and environmental data, indicate dry and cool conditions prior and during the initial phase of the settlement formation. The abandonment of the settlement, possibly in the late 5th millennium, probably occurred due to alternating dry and wet episodes, rather than a gradual increase in wet conditions, as suggested elsewhere in the region. A large ditch encircling the settlement, not documented by archaeological research, can be indirectly confirmed by the BR2 core results and the analysis of aerial and satellite images. In general, there is a good correlation of results with the major global climate events, but there are differences in regional and wider south-eastern European context.^aarcheological record^aenvironmental change^afreshwater fauna^asoil chemistry^asouthern Carpathian Basin
Słowa kluczowe ang.:
Streszczenie:

2/10
Nr opisu: naRychel Joanna Sokołowski Robert J. Sieradz Dominika Hrynowiecka Anna Mirosław-Grabowska Joanna Sienkiewicz Elwira^aoriginal-article^bOryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym1.900IF^a997000^b998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM^a009997.100^b009899.000^c009999.000^d009899.000202320232023Late Pleniglacial - Late Glacial climate oscillations detected in the organic lacustrine successi00000443510000000358AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttps://onlinelibrary.wiley.com/doi/10.1002/jqs.3477100^a0267-8179^bQ^e1099-1417^iX^jXY^kQ012470^a003^b003^c2022-11-08, 13:07^d2024-06-25, 14:14^e3219968932^f3024798825^aLate Pleniglacial - Late Glacial climate oscillations detected in the organic lacustrine succession at the Lipowo site, north-eastern Poland^aJournal of Quaternary Science^a2023^bVol. 38^cissue 2^dp. 186--207^a1099-1417^b1099-1417^a2022/2023^a10.1002/jqs.3477^aZbucki, Łukasz^cx^ablock melting^aThe profile of the Lipowo palaeolake (NE Poland) preserves a record of environmental and climate changes from the Last Glacial Termination (16.5k cal ka BP), stretching from the Oldest Dryas to the youngest Allerod warm oscillation. In this interdisciplinary study of the lacustrine succession at Lipowo, we used biological and geochemical indicators and multiproxy analyses to reconstruct environmental changes in the lake ecosystem, such as mollusc, zooplankton and vegetation development, trophic state, water temperature and water level. Four cold and four warm climate oscillations of different durations were identified on this basis: the Older Dryas climate deterioration and two short-term coolings within the Allerod Interstadial, separated by warm periods in the Bolling and Allerod. The covering of the lake series by diamicton deposits from the melting of dead-ice blocks is a particularly interesting and rare phenomenon for a postglacial area. The hydrological system of the catchment was generally closed, with a periodically opening and existing flow-through lake. Over the period of the lake's existence, vegetation changed in general from steppe tundra to forest with birch and pine. For most of this time, the palaeolake was mainly oligotrophic, with increased productivity and a higher trophic level only notable during the middle Bolling.^adead-ice^aLast Glacial Termination^apalaeoenvironment reconstruction^apermafrost^apollen analysis
Autorzy: , , .
Tytuł pracy:
Tytuł pracy w innym języku: NiskaSzymanekZbuckiCiołkoRogóż-Matyszczakoriginal-article997000009997.1000267-8179003Late Pleniglacial - Late Glacial climate oscillations detected in the organic lacustrine succession at the Lipowo site, north-eastern PolandJournal of Quaternary Science20231099-14172022/202310.1002/jqs.3477Zbucki, Łukaszblock meltingThe profile of the Lipowo palaeolake (NE Poland) preserves a record of environmental and climate changes from the Last Glacial Termination (16.5k cal ka BP), stretching from the Oldest Dryas to the youngest Allerod warm oscillation. In this interdisciplinary study of the lacustrine succession at Lipowo, we used biological and geochemical indicators and multiproxy analyses to reconstruct environmental changes in the lake ecosystem, such as mollusc, zooplankton and vegetation development, trophic state, water temperature and water level. Four cold and four warm climate oscillations of different durations were identified on this basis: the Older Dryas climate deterioration and two short-term coolings within the Allerod Interstadial, separated by warm periods in the Bolling and Allerod. The covering of the lake series by diamicton deposits from the melting of dead-ice blocks is a particularly interesting and rare phenomenon for a postglacial area. The hydrological system of the catchment was generally closed, with a periodically opening and existing flow-through lake. Over the period of the lake's existence, vegetation changed in general from steppe tundra to forest with birch and pine. For most of this time, the palaeolake was mainly oligotrophic, with increased productivity and a higher trophic level only notable during the middle Bolling.dead-iceLast Glacial Terminationpalaeoenvironment reconstructionpermafrostpollen analysis : Monika : Marcin : Łukasz Jan : Urszula : Anna : Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym1.900IF : 998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM : 009899.000 : Q : 003 : Vol. 38 : 1099-1417
Oznaczenie wydania: NiskaSzymanekZbucki
Charakterystyka formalna:
Słowa kluczowe ang.: ;

3/10
Nr opisu: 0^b998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM^a009996.700^b009899.000^c009999.000^d009899.000202220222022High-resolution insight into the Holocene environmental history of the Burullus Lagoon in norther00000426000000000609AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttps://www.cambridge.org/core/journals/quaternary-research/article/abs/highresolution-insight-into-the-holocene-environmental-history-of-the-burullus-lagoon-in-northern-nile-delta-egypt/B3B5C71601138100^a0033-5894^bQ^e1096-0287^fA^hABC^iX^jXY^kQ016946^a003^b003^c2021-12-01, 14:27^d2023-06-28, 10:07^e3319038812^f3124769232^aHigh-resolution insight into the Holocene environmental history of the Burullus Lagoon in northern Nile delta, Egypt^aQuaternary Research^a2022^bVol. 107^dp. 87--103^a0033-5894^b1096-0287^a2021/2022^a10.1017/qua.2021.63^aNitychoruk, Jerzy^cy^aclimate change^aFINAL_PUBLISHED^bCC-BY-NC-ND^cAT_PUBLICATION^eOPEN_JOURNAL^aThe modern Nile delta developed in the Middle and Late Holocene, and at its most northern-central point is situated at the Burullus Lagoon, which is environmentally diverse, including salt marshes, mudflats, and sand plains, and separated from a sea by a sand barrier overtopped with high sand dunes. The lagoon has been fed since the Middle Holocene by the Sebennitic branch of the Nile and marine intrusions through the Bughaz inlet. A sediment core (BO-1) was collected at the northeastern shore of the lagoon and sampled at centennial scale resolution in order to reconstruct the development of the lagoon. The results show that an initial and limited lagoon had developed at the end of the Early Holocene, but after a dry period ca. 7.2 cal ka BP it has been progressively transformed into a marshy area, with occasional inflows of sea water. Lower water level and higher salinity of the Burullus Lagoon at 6.0-5.5 and 4.8-4.2 cal ka BP reflected droughts in the Nile catchment. Thereafter, the river reactivated in the Burullus Lagoon area, and since 2.8 cal ka BP was accompanied by occasional inflows of sea water. Since ca. 0.8 cal ka BP, increased fluvial activity occurred in this part of the Nile delta, which terminated after construction of the Aswan dams in the twentieth century.^aEastern Mediterranean^aIntertropical Convergence Zone^alagoon^aNile delta^asea-level change^aSebennitic branch.300IF^a996600^b998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM^a009996.700^b009899.000^c009999.000^d009899.000202220222022High-resolution insight into the Holocene environmental history of the Burullus Lagoon in norther00000426000000000609AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttps://www.cambridge.org/core/journals/quaternary-research/article/abs/highresolution-insight-into-the-holocene-environmental-history-of-the-burullus-lagoon-in-northern-nile-delta-egypt/B3B5C71601138100^a0033-5894^bQ^e1096-0287^fA^hABC^iX^jXY^kQ016946^a003^b003^c2021-12-01, 14:27^d2023-06-28, 10:07^e3319038812^f3124769232^aHigh-resolution insight into the Holocene environmental history of the Burullus Lagoon in northern Nile delta, Egypt^aQuaternary Research^a2022^bVol. 107^dp. 87--103^a0033-5894^b1096-0287^a2021/2022^a10.1017/qua.2021.63^aNitychoruk, Jerzy^cy^aclimate change^aFINAL_PUBLISHED^bCC-BY-NC-ND^cAT_PUBLICATION^eOPEN_JOURNAL^aThe modern Nile delta developed in the Middle and Late Holocene, and at its most northern-central point is situated at the Burullus Lagoon, which is environmentally diverse, including salt marshes, mudflats, and sand plains, and separated from a sea by a sand barrier overtopped with high sand dunes. The lagoon has been fed since the Middle Holocene by the Sebennitic branch of the Nile and marine intrusions through the Bughaz inlet. A sediment core (BO-1) was collected at the northeastern shore of the lagoon and sampled at centennial scale resolution in order to reconstruct the development of the lagoon. The results show that an initial and limited lagoon had developed at the end of the Early Holocene, but after a dry period ca. 7.2 cal ka BP it has been progressively transformed into a marshy area, with occasional inflows of sea water. Lower water level and higher salinity of the Burullus Lagoon at 6.0-5.5 and 4.8-4.2 cal ka BP reflected droughts in the Nile catchment. Thereafter, the river reactivated in the Burullus Lagoon area, and since 2.8 cal ka BP was accompanied by occasional inflows of sea water. Since ca. 0.8 cal ka BP, increased fluvial activity occurred in this part of the Nile delta, which terminated after construction of the Aswan dams in the twentieth century.^aEastern Mediterranean^aIntertropical Convergence Zone^alagoon^aNile delta^asea-level change^aSebennitic branch
Autorzy: , , .
Tytuł pracy:
Tytuł pracy w innym języku: NitychorukChenSalemZalatoriginal-article996600009996.7000033-5894003High-resolution insight into the Holocene environmental history of the Burullus Lagoon in northern Nile delta, EgyptQuaternary Research20220033-58942021/202210.1017/qua.2021.63Nitychoruk, Jerzyclimate changeFINAL_PUBLISHEDThe modern Nile delta developed in the Middle and Late Holocene, and at its most northern-central point is situated at the Burullus Lagoon, which is environmentally diverse, including salt marshes, mudflats, and sand plains, and separated from a sea by a sand barrier overtopped with high sand dunes. The lagoon has been fed since the Middle Holocene by the Sebennitic branch of the Nile and marine intrusions through the Bughaz inlet. A sediment core (BO-1) was collected at the northeastern shore of the lagoon and sampled at centennial scale resolution in order to reconstruct the development of the lagoon. The results show that an initial and limited lagoon had developed at the end of the Early Holocene, but after a dry period ca. 7.2 cal ka BP it has been progressively transformed into a marshy area, with occasional inflows of sea water. Lower water level and higher salinity of the Burullus Lagoon at 6.0-5.5 and 4.8-4.2 cal ka BP reflected droughts in the Nile catchment. Thereafter, the river reactivated in the Burullus Lagoon area, and since 2.8 cal ka BP was accompanied by occasional inflows of sea water. Since ca. 0.8 cal ka BP, increased fluvial activity occurred in this part of the Nile delta, which terminated after construction of the Aswan dams in the twentieth century.Eastern MediterraneanIntertropical Convergence ZonelagoonNile deltasea-level changeSebennitic branch : Jerzy Antoni : Zhongyuan : Alaa : Abdelfattah : Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym2.300IF : 998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM : 009899.000 : Q : 003 : Vol. 107 : 1096-0287 : CC-BY-NC-ND
Miejsce wydania: NitychorukChenSalemZalatoriginal-article996600009996.7000033-5894003High-resolution insight into the Holocene environmental history of the Burullus Lagoon in northern Nile delta, EgyptQuaternary Research20220033-58942021/202210.1017/qua.2021.63Nitychoruk, Jerzyclimate changeFINAL_PUBLISHEDThe modern Nile delta developed in the Middle and Late Holocene, and at its most northern-central point is situated at the Burullus Lagoon, which is environmentally diverse, including salt marshes, mudflats, and sand plains, and separated from a sea by a sand barrier overtopped with high sand dunes. The lagoon has been fed
Wydawca: Jerzy AntoniZhongyuanAlaaAbdelfattahOryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym2.300IF998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM009899.000Q003Vol. 1071096-0287CC-BY-NC-ND
Rok wydania: 033009999.0002021-12-01, 14:27yAT_PUBLICATION
Strony: NitychorukChenSalemZalatoriginal-article996600009996.7000033-5894003High-resolution insight into the Holocene environmental history of the Burullus Lagoon in northern Nile delta, EgyptQuaternary Research20220033-58942021/202210.1017/qua.2021.63Nitychoruk, Jerzyclimate changeFINAL_PUBLISHEDThe modern Nile delta developed in the Middle and Late Holocene, and at its most northern-central point is situated at the Burullus Lagoon, which is environmentally diverse, including salt marshes, mudflats, and sand plains, and separated from a sea by a sand barrier overtopped with high sand dunes. The lagoon has been fed since the Middle Holocene by the Sebennitic branch of the Nile and marine intrusions through the Bughaz inlet. A sediment core (BO-1) was collected at the northeastern shore of the lagoon and sampled at centennial scale resolution in order to reconstruct the development of the lagoon. The results show that an initial and limited lagoon had developed at the end of the Early Holocene, but after a dry period ca. 7.2 cal ka BP it has been progressively transformed into a marshy area, with occasional inflows of sea water. Lower water level and higher salinity, Jerzy Antoni, Zhongyuan, Alaa, Abdelfattah, Oryginalny artykuł naukowyACZartykuł w czasopiśmie zagranicznym2.300IF, 998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM, 009899.000, Q, 003, Vol. 107, 1096-0287, CC-BY-NC-ND, 033, , , , 009999.000, 2021-12-01, 14:27, y, AT_PUBLICATION, WNET0201, , , , 009899.000202220222022High-resolution insight into the Holocene environmental history of the Burullus Lagoon in norther00000426000000000609AOartykuł oryginalny naukowyPUBLIKACJAPEŁNA PUBLIKACJAAAartykuł w czasopiśmie z IF (wykaz MNiSW)AFILIACJA PODANAENGhttps://www.cambridge.org/core/journals/quaternary-research/article/abs/highresolution-insight-into-the-holocene-environmental-history-of-the-burullus-lagoon-in-northern-nile-delta-egypt/B3B5C71601138100, 2023-06-28, 10:07, p. 87--103
Charakterystyka formalna:
Słowa kluczowe ang.: ;
Streszczenie:

4/10
Autorzy: , , .
Szczegóły:
Tytuł monografii w innym języku: 994401009994.5021814-93240032400 years of climate and human-induced environmental change recorded in sediments of Lake Młynek in northern PolandClimate of the Past20211814-93242020/202110.5194/cp-17-1181-2021climate changeKorelacja faz osadnictwa pradziejowego i wczesnośredniowiecznego w Polsce północno-wschodniej z przemianami środowiska przyrodniczego w świetle badań osadów jeziornych (Correlation of prehistoric and early medieval settlement phases in northeast Poland with the changes of the natural environment in the light of lacus-trine sediments study)FINAL_PUBLISHEDIn the densely forested Warmia and Masuria region (northern Poland) there are many small endorheic lakes characterized by their low sedimentation rate, which makes them excellent archives of Holocene environmental and palaeoclimatic change. Lake Młynek, located near the village of Janiki Wielkie, was selected for multi-faceted palaeoenvironmental research supported with radiocarbon dates. Sediments from this lake also contain unique information about human impact on the environment, because a stronghold has been operating on its northern shore since the early Iron Age to the early Medieval period, giving the opportunity to correlate palaeoenvironmental data with the phases of human activity over the last 2400 years. : 998999100.0000100.000PUNKTACJA KBNPUNKTACJA MINISTERSTWALISTA FILADELFIJSKAIMPACT FACTOR100.000PUNKTACJA UWM : 009899.000 : Q : 003 : Vol. 17 : 1814-9332 : UMO-2016/21/B/ST10/03059 : CC-BY
Charakterystyka formalna: dowiska przyrodniczego w świetle badań osadów jeziornych (Correlation of prehistoric and early medieval settlement phases in northeast Poland with the changes of the natural environment in the light of lacus-trine sediments study)^bUMO-2016/21/B/ST10/03059^d2017-2022^aFINAL_PUBLISHED^bCC-BY^cAT_PUBLICATION^eOPEN_JOURNAL^aIn the densely forested Warmia and Masuria region (northern Poland) there are many small endorheic lakes characterized by their low sedimentation rate, which makes them excellent archives of Holocene environmental and palaeoclimatic change. Lake Młynek, located near the village of Janiki Wielkie, was selected for multi-faceted palaeoenvironmental research supported with radiocarbon dates. Sediments from this lake also contain unique information about human impact on the environment, because a stronghold has been operating on its northern shore since the early Iron Age to the early Medieval period, giving the opportunity to correlate palaeoenvironmental data with the phases of human activity over the last 2400 years. During the second and third centuries BCE the lake was surrounded by a dense deciduous forest. From the first century BCE to second century CE the forest around the lake was much reduced, which can be associated with the first pre-Roman (La Tene) and Roman occupation phase evidenced by the construction of the stronghold located close to the lake. From the second up to ninth century CE gradual restoration of the forest and a decline in human activity took place, along with lake deepening and the onset of a colder and humid climatic phase which corresponded to the global cooling episode known as the Bond 1 event (1.5 ka BP). The next intensive phase of forest clearing around the lake occurred between the 9th-13th century CE as result of human activity (Middle Age settlement phase of the stronghold). Whilst this period is marked by a warming, the human impact which has transformed the landscape likely overprints any signals of climate-driven environmental changes.^aenvironmental change^alake sediments^aholocene^amiddle age^ahuman activity^aLake Młynek^aPoland
Charakterystyka wg MNiSW:
Język publikacji: przyrodniczego w świetle badań osadów jeziornych (Correlation of prehistoric and early medieval settlement phases in northeast Poland with the changes of the natural environment in the light of lacus-trine sediments study)^bUMO-2016/21/B/ST10/03059^d2017-2022^aFINAL_PUBLISHED^bCC-BY^cAT_PUBLICATION^eOPEN_JOURNAL^aIn the densely forested Warmia and Masuria region (northern Poland) there are many small endorheic lakes characterized by their low sedimentation rate, which makes them excellent archives of Holocene environmental and palaeoclimatic change. Lake Młynek, located near the village of Janiki Wielkie, was selected for multi-faceted palaeoenvironmental research supported with radiocarbon dates. Sediments from this lake also contain unique information about human impact on the environment, because a stronghold has been operating on its northern shore since the early Iron Age to the early Medieval period, giving the opportunity to correlate palaeoenvironmental data with the phases of human activity over the last 2400 years. During the second and third centuries BCE the lake was surrounded by a dense deciduous forest. From the first century BCE to second century CE the forest around the lake was much reduced, which can be associated with the first pre-Roman (La Tene) and Roman occupation phase evidenced by the construction of the stronghold located close to the lake. From the second up to ninth century CE gradual restoration of the forest and a decline in human activity took place, along with lake deepening and the onset of a colder and humid climatic phase which corresponded to the global cooling episode known as the Bond 1 event (1.5 ka BP). The next intensive phase of forest clearing around the lake occurred between the 9th-13th century CE as result of human activity (Middle Age settlement phase of the stronghold). Whilst this period is marked by a warming, the human impact which has transformed the landscape likely overprints any signals of climate-driven environmental changes.^aenvironmental change^alake sediments^aholocene^amiddle age^ahuman activity^aLake Młynek^aPoland
Słowa kluczowe ang.: ;

DOI:

5/10
Nr opisu: River terraces in the Neple area (Podlasie Lowland, eastern Poland)^aBaltica^a2020^bVol. 33^cno 1^dp. 1--10^a0067-3064^b1648-858X^a2019/2020^a10.5200/baltica.2020.1.1^aZbucki, Łukasz^cx^ahuman impact^aFINAL_PUBLISHED^bOTHER^cAT_PUBLICATION^eOPEN_JOURNAL^aThe gullies in the vicinity of Neple (Podlaska Lowland, eastern Poland) are relatively young and were created due to the land use and climate changes. The aim of the research was to determine the variability of selected alluvial-diluvial fans occurring in the Bug River valley and their age using interdisciplinary methods (e.g. absolute dating, geochemical analyzes, cartographic data). Geological mapping and several drillings (both within the fans, valleys or gullies bottoms and glacial or fluvioglacial plateaus) were done. Historical data dealing with the human economic activity in the region were analyzed. The obtained radiocarbon dating and geochemical features of sediments building the alluvial and diluvial fans proved that these forms are not older than some 500 years. Due to the lateral movement of the Bug River channel only some of the forms are preserved in the area under study. The rest of them disappeared due to the fluvial erosion.^atrace elements^aland use changes^agully erosion^aradiocarbon dating
Autorzy: , Vol. 33 1648-858X OTHER Baltica20200067-30642019/202010.5200/baltica.2020.1.1Zbucki, Łukaszhuman impactFINAL_PUBLISHEDThe gullies in the vicinity of Neple (Podlaska Lowland, eastern Poland) are relatively young and were created due to the land use and climate changes. The aim of the research was to determine the variability of selected alluvial-diluvial fans occurring in the Bug River valley and their age using interdisciplinary methods (e.g. absolute dating, geochemical analyzes, cartographic data). Geological mapping and several drillings (both within the fans, valleys or gullies bottoms and glacial or fluvioglacial plateaus) were done. Historical data dealing with the human economic activity in the region were analyzed. The obtained radiocarbon dating and geochemical features of sediments building the alluvial and diluvial fans proved that these forms are not older than some 500 years. Due to the lateral movement of the Bug River channel only some of the forms are preserved in the area under study. The rest of them disappeared due to the fluvial erosion.trace elementsland use changesgully erosionradiocarbon dating, Vol. 33 1648-858X OTHER Baltica20200067-30642019/202010.5200/baltica.2020.1.1Zbucki, Łukaszhuman impactFINAL_PUBLISHEDThe gullies in the vicinity of Neple (Podlaska Lowland, eastern Poland) are relatively young and were created due to the land use and climate changes. The aim of the research was to determine the variability of selected alluvial-diluvial fans occurring in the Bug River valley and their age using interdisciplinary methods (e.g. absolute dating, geochemical analyzes, cartographic data). Geological mapping and several drillings (both within the fans, valleys or gullies bottoms and glacial or fluvioglacial plateaus) were done. Historical data dealing with the human economic activity in the region were analyzed. The obtained radiocarbon dating and geochemical features of sediments building the alluvial and diluvial fans proved that these forms are not older than some 500 years. Due to the lateral movement of the Bug River channel only some of the forms are preserved in the area under study. The rest of them disappeared due to the fluvial erosion.trace elementsland use changesgully erosionradiocarbon dating.
Tytuł czasopisma:
Charakterystyka merytoryczna:
Język publikacji:
Wskaźnik Impact Factor ISI:
Punktacja ministerstwa:
Praca recenzowana
Słowa kluczowe ang.: ; ;

6/10
Nr opisu: alley^aJakość i znaczenie wód gruntowych w strefie krawędziowej Doliny Bugu^aHealth Problems of Civilization^a2020^bVol. 14^cissue 4^dp. 320--326^a2353-6942^b2354-0265^a2020/2021^a10.5114/hpc.2020.97679^ageochemia wód^awater geochemistry^aFINAL_PUBLISHED^bCC-BY-NC-SA^cBEFORE_PUBLICATION^eOPEN_JOURNAL^aThe use of groundwater from private wells in households is increasing significantly. However, this water is usually untreated, making it a carrier of diseases. Chemical composition plays a key role in assessing groundwater quality. Due to rapid urbanization and industrialization of the environment, pollutants (especially toxic elements) are constantly being released into the aquatic environment and pose a threat to human and animal health. There is a large variety of microorganisms in aquifers. The use of groundwater from aquifers as sources of drinking water without water treatment or disinfection is a public health problem. Material and methods: The material for the study consisted of water samples taken from used and unused domestic wells in villages located in Lubelskie Province, Biała Podlaska County, Janów Podlaski municipality, Poland. ICP-OES was used to determine the composition of elements. The total number of mesophilic and psychrophilic bacteria was determined for 5 wells using the pour-plate method according to the Polish Standard PN-EN ISO 6222:2004. Results: The water from the wells is unfit for consumption due to high microbiological contamination. A study would have to be carried out on the content of specific pathogenic microorganisms. In most of the samples analyzed, the heavy metal content of the water is below admissible limits. Conclusions: Water resources of the highest quality should be increasingly protected and retained as drinking water reserves. This is extremely important in view of the progressing climate change and the slow process of groundwater renewal.^ahydrologia^ahydrology^aZużycie wody gruntowej ze studni prywatnych w gospodarstwach domowych znacznie wzrasta. Jednakże
Autorzy: , , Vol. 14 2354-0265 CC-BY-NC-SA Jakość i znaczenie wód gruntowych w strefie krawędziowej Doliny BuguHealth Problems of Civilization20202353-69422020/202110.5114/hpc.2020.97679geochemia wódwater geochemistryFINAL_PUBLISHEDThe use of groundwater from private wells in households is increasing significantly. However, this water is usually untreated, making it a carrier of diseases. Chemical composition plays a key role in assessing groundwater quality. Due to rapid urbanization and industrialization of the environment, pollutants (especially toxic elements) are constantly being released into the aquatic environment and pose a threat to human and animal health. There is a large variety of microorganisms in aquifers. The use of groundwater from aquifers as sources of drinking water without water treatment or disinfection is a public health problem. Material and methods: The material for the study consisted of water samples taken from used and unused domestic wells in villages located in Lubelskie Province, Biała Podlaska County, Janów Podlaski municipality, Poland. ICP-OES was used to determine the composition of elements. The total number of mesophilic and psychrophilic bacteria was determined for 5 wells using the pour-plate method according to the Polish Standard PN-EN ISO 6222:2004. Results: The water from the wells is unfit for consumption due to high microbiological contamination. A study would have to be carried out on the content of specific pathogenic microorganisms. In most of the samples analyzed, the heavy metal content of the water is below admissible limits. Conclusions: Water resources of the highest quality should be increasingly protected and retained as drinking water reserves. This is extremely important in view of the progressing climate change and the slow process of groundwater renewal.hydrologiahydrologyZuż.
Tytuł pracy:
Szczegóły:
Tytuł całości: W: Jakość i znaczenie wód gruntowych w strefie krawędziowej Doliny BuguHealth Problems of Civilization2020 : Vol. 14 / issue 4
Punktacja ministerstwa:
Słowa kluczowe ang.: or disinfection is a public health problem. Material and methods: The material for the study consisted of water samples taken from used and unused domestic wells in villages located in Lubelskie Province, Biała Podlaska County, Janów Podlaski municipality, Poland. ICP-OES was used to determine the composition of elements. The total number of mesophilic and psychrophilic bacteria was determined for 5 wells using the pour-plate method according to the Polish Standard PN-EN ISO 6222:2004. Results: The water from the wells is unfit for consumption due to high microbiological contamination. A study would have to be carried out on the content of specific pathogenic microorganisms. In most of the samples analyzed, the heavy metal content of the water is below admissible limits. Conclusions: Water resources of the highest quality should be increasingly protected and retained as drinking water reserves. This is extremely important in view of the progressing climate change and the slow process of groundwater renewal.^ahydrologia^ahydrology^aZużycie wody gruntowej ze studni prywatnych w gospodarstwach domowych znacznie wzrasta. Jednakże woda ta jest zwykle nieoczyszczona, co czyni ją nośnikiem chorób. W ocenie jakości wód podziemnych kluczową rolę odgrywa skład chemiczny. Z powodu szybkiej urbanizacji i uprzemysłowienia środowiska, zanieczyszczenia (zwłaszcza toksyczne pierwiastki) są stale uwalniane do środowiska wodnego i stanowią zagrożenie dla zdrowia ludzi i zwierząt. W warstwach wodonośnych występuje duża różnorodność mikroorganizmów. Problemem zdrowia publicznego jest wykorzystywanie warstw wodonośnych wód podziemnych jako źródeł wody pitnej bez procesu oczyszczania wody lub dezynfekcji. Materiał i metody: Materiał do badań stanowiły próby wody pobrane z użytkowanych i nieużytkowanych studni przydomowych we wsiach położonych w województwie lubelskim, powiecie bialskim, w gminie Janów Podlaski. W celu oznaczenia zawartości pierwiastków wykorzystano metodę ICP-OES. Dla 5 studni określono ogólną liczbę bakterii mezofilnych i psychrofilnych przy wykorzystaniu metody płytek lanych zgodnie z Polską Normą PN-EN ISO 6222:2004. Wyniki: Woda pochodząca ze studni nie nadaje się do spożycia z uwagi na wysokie zanieczyszczanie mikrobiologiczne. Konieczne byłoby przeprowadzenie badania na zawartość konkretnych mikroorganizmów chorobotwórczych. W większości analizowanych prób zawartość metali ciężkich w wodzie znajduje się poniżej dopuszczalnej granicy. Wnioski: Zasoby wodne o najwyższej jakości powinny być poddane coraz większej ochronie i pozostawione jako rezerwa wód pitnych. Jest to niezwykle istotne z uwagi na postępującą zmianę klimatu oraz powolny proces odnawiania wód podziemnych.^amikrobiologia wód^awater microbiology^astudnie przydomowe^adomestic wells^awody podziemne^agroundwater^adolina Bugu^awater pollution^azanieczyszczenie wody^aBug valley
Słowa kluczowe:
Słowa kluczowe ang.: ; ;
DOI:

7/10
Nr opisu: _PUBLICATION^eOPEN_JOURNAL^aA field experiment was conducted in Międzyrzec Podlaski, (51o59' N and 22o47' E), Poland in the period from 2015 to 2017. The experiment was a two-way random split-plot arrangement of plots with three replicates. The following factors were examined: three varieties of potato - - Honorata, Jelly, Tajfun, and four variants of application of biostimulants (Kelpak SL, Titanit, GreenOk, BrunatneBio Złoto). The control object was comprised plants potato plants sprayed with distilled water. Biostimulators were applied to potato plants three times (beginning of flowering, full flowering and after flowering of the plants). The aim of the study was to determine the effect of biostimulants on the content and uptake of zinc and copper with the yield of potato tubers. High amount of rainfall in 2017 contributed to an increase in the content of zinc and copper in potato tubers. The tubers of potatoes treated with BrunatneBio Złoto had the highest contenting uptake of Zn and Cu compared to the control plants. The content of microelements in the tubers was significantly dependent on the genotype. The highest concentrations of Zn and Cu was were found in the Honorata tubers of the Honorata, and the lar
Autorzy: CC-BY FINAL_PUBLISHEDA field experiment was conducted in Międzyrzec Podlaski, (51o59' N and 22o47' E), Poland in the period from 2015 to 2017. The experiment was a two-way random split-plot arrangement of plots with three replicates. The following factors were examined: three varieties of potato - - Honorata, Jelly, Tajfun, and four variants of application of biostimulants (Kelpak SL, Titanit, GreenOk, BrunatneBio Złoto). The control object was comprised plants potato plants sprayed with distilled water. Biostimulators were applied to potato plants three times (beginning of flowering, full flowering and after flowering of the plants). The aim of the study was to determine the effect of biostimulants on the content and uptake of zinc and copper with the yield of potato tubers. High amount of rainfall in 2017 contributed to an increase in the content of zinc and copper in potato tubers. The tubers of potatoes treated with BrunatneBio Złoto had the highest contenting uptake of Zn and Cu compared to the control plants. The content of microelements in the tubers was significantly dependent on the genotype. The highest c.
Tytuł pracy: FINAL_PUBLISHEDA field experiment was conducted in Międzyrzec Podlaski, (51o59' N and 22o47' E), Poland in the period from 2015 to 2017. The experiment was a two-way random split-plot arrangement of plots with three replicates. The following factors were examined: three varieties of potato - - Honorata, Jelly, Tajfun, and four variants of application of biostimulants (Kelpak SL, Titanit, GreenOk, BrunatneBio Złoto). The control object was comprised plants potato plants sprayed with distilled water. Biostimulators were applied to potato plants three times (beginning of flowering, full flowering and after flowering of the plants). The aim of the study was to determine the effect of biostimulants on the content and uptake of zinc and copper with the yield of potato tubers. High amount of rainfall in 2017 contributed to an increase in the content of zinc and copper in potato tubers. The tubers of potatoes treated with BrunatneBio Złoto had the highest contenting uptake of Zn and Cu compared to the control plants. The content of microelements in the tubers was significantly dependent on the genotype. The highest concentrations of Zn and Cu was were found in the Honorata tubers of the Honorata, and the largest uptake was observed in athe Jelly variety Jelly.Solanum tuberosum varietieszinccopper : CC-BY, OPEN_JOURNAL
Szczegóły:
Miejsce: FINAL_PUBLISHEDA field experiment was conducted in Międzyrzec Podlaski, (51o59' N and 22o47' E), Poland in the period from 2015 to : CC-BY, AT_PUBLICATION
Punktacja ministerstwa:
Index Copernicus: a bioregulatorów i herbicydów^aFINAL_PUBLISHED^bCC-BY^cAT_PUBLICATION^eOPEN_JOURNAL^aA field experiment was conducted in Międzyrzec Podlaski, (51o59' N and 22o47' E), Poland in the period from 2015 to 2017. The experiment was a two-way random split-plot arrangement of plots with three replicates. The following factors were examined: three varieties of potato - - Honorata, Jelly, Tajfun, and four variants of application of biostimulants (Kelpak SL, Titanit, GreenOk, BrunatneBio Złoto). The control object was comprised plants potato plants sprayed with distilled water. Biostimulators were applied to potato plants three times (beginning of flowering, full flowering and after flowering of the plants). The aim of the study was to determine the effect of biostimulants on the content and uptake of zinc and copper with the yield of potato tubers. High amount of rainfall in 2017 contributed to an increase in the content of zinc and copper in potato tubers. The tubers of potatoes treated with BrunatneBio Złoto had the highest contenting uptake of Zn and Cu compared to the control
Praca recenzowana
Słowa kluczowe ang.: dów^aFINAL_PUBLISHED^bCC-BY^cAT_PUBLICATION^eOPEN_JOURNAL^aA field experiment was conducted in Międzyrzec Podlaski, (51o59' N and 22o47' E), Poland in the period from 2015 to 2017. The experiment was a two-way random split-plot arrangement of plots with three replicates. The following factors were examined: three varieties of potato - - Honorata, Jelly, Tajfun, and four variants of application of biostimulants (Kelpak SL, Titanit, GreenOk, BrunatneBio Złoto). The control object was comprised plants potato plants sprayed with distilled water. Biostimulators were applied to potato plants three times (beginning of flowering, full flowering and after flowering of the plants). The aim of the study was to determine the effect of biostimulants on the content and uptake of zinc and copper with the yield of potato tubers. High amount of rainfall in 2017 contributed to an increase in the content of zinc and copper in potato tubers. The tubers of potatoes treated with BrunatneBio Złoto had the highest contenting uptake of Zn and Cu compared to the control plants. The content of microelements in the tubers was significantly dependent on the genotype. The highest concentrations of Zn and Cu was were found in the Honorata tubers of the Honorata, and the largest uptake was observed in athe Jelly variety Jelly.^aSolanum tuberosum varieties^azinc^acopper
Słowa kluczowe ang.:
Uwaga:
DOI:
Streszczenie:

8/10
Nr opisu: 
Tytuł całości: W:
Miejsce: Content and uptake of selected microelements with potato tuber yield treated with biostimulatorsForum2019 : 10th Forum of Ecological Engineering, 9-11 September 2019, Kazimierz Doln,
Wskaźnik Impact Factor ISI:
Index Copernicus: 14:20^e3521918819^f3521918819^aContent and uptake of selected microelements with potato tuber yield treated with biostimulators^aForum2019^b10th Forum of Ecological Engineering, 9-11 September 2019, Kazimierz Dolny, Polamd : book of abstracts^aS. 92^aLublin^bLublin University of Technology^c2019^aMystkowska, Iwona^cy^ayield^aKopia dostępna w Sekcji Bibliometrii.^a10th Forum of Ecological Engineering^aKazimierz Dolny^dPL^b2019.08.09^c2019.08.11^apotato^amicroelements
Słowa kluczowe ang.:

9/10
Nr opisu: of biostimulators in individual farms in the town of Międzyrzec Podlaski (51°59' N and 22°47' E), Poland. The experiment was led by means of a split-plot method. The impact of two factors was tested. The first order factor were the three varieties of edible potato: Honorata, Jelly, Tajfun, while of the second order - four variants of applying biostimulators: Kelpak SL, Titanit, GreenOk, BrunatneBio Złoto and a control variant (potato plants sprayed with distilled water). Potato plants were treated with biostimulators three times (beginning of flowering, full flowering and after plant flowering). Within the presented research the applied biostimulators increased the content of selected mineral components in the tubers of tested varieties. Tubers of plants treated with BrunatneBio Złoto preparation were characterized by the largest content of phosphorus, calcium and magnesium in comparison to the plants from control object. The content of microelements in the tubers varied significantly depending on the genotype of the variety. The greatest concentration of phosphorus was noted in the tubers of Tajfun variety, while in case of magnesium - Honorata variety. Large amount of rainfall in 2017 contributed to the occurrence of an increase of the content of phosphorus, calcium and magnesium in potato tubers. Average content of phosphorus amount to, on average: 3.4 g•kg-1, calcium 0.73 g•kg-1 , and magnesium 1.36 g•kg-1.^avariety^aphosphorus^acalcium^amagnesium application of biostimulators in individual farms in the town of Międzyrzec Podlaski (51°59' N and 22°47' E), Poland. The experiment was led by means of a split-plot method. The impact of two factors was tested. The first order factor were the three varieties of edible potato: Honorata, Jelly, Tajfun, while of the second order - four variants of applying biostimulators: Kelpak SL, Titanit, GreenOk, BrunatneBio Złoto and a control variant (potato plants sprayed with distilled water). Potato plants were treated with biostimulators three times (beginning of flowering, full flowering and after plant flowering). Within the presented research the applied biostimulators increased the content of selected mineral components in the tubers of tested varieties. Tubers of plants treated with BrunatneBio Złoto preparation were characterized by the largest content of phosphorus, calcium and magnesium in comparison to the plants from control object. The content of microelements in the tubers varied significantly depending on the genotype of the variety. The greatest concentration of phosphorus was noted in the tubers of Tajfun variety, while in case of magnesium - Honorata variety. Large amount of rainfall in 2017 contributed to the occurrence of an increase of the content of phosphorus, calcium and magnesium in potato tubers. Average content of phosphorus amount to, on average: 3.4 g•kg-1, calcium 0.73 g•kg-1 , and magnesium 1.36 g•kg-1.^avariety^aphosphorus^acalcium^amagnesium
Autorzy: , Q 003 Vol. 17 1785-0037 UPH Siedlce / MNiSW w ramach środków przekazywanych jednostkom na finansowanie działalności statutowej OTHER 1589-1623003Content of the selected macro-elements in potato tubers (Solanum tuberosum L.) treated with biostimulatorsApplied Ecology and Environmental Research20191589-16232018/201910.15666/aeer/1705_1192511933Mystkowska, IwonavariantKopia dostępna w Sekcji Bibliometrii.Badania statutoweFINAL_PUBLISHEDThe objective of research was to assess the selected mineral components (phosphorus, calcium and magnesium) in the tubers of edible potato. Field research was carried out in the years 2015-2017 with an application of biostimulators in individual farms in the town of Międzyrzec Podlaski (51°59' N and 22°47' E), Poland. The experiment was led by means of a split-plot method. The impact of two factors was tested. The first order factor were the three varieties of edible potato: Honorata, Jelly, Tajfun, while of the second order - four variants of applying biostimulators: Kelpak SL, Titanit, GreenOk, BrunatneBio Złoto and a control variant (potato plants sprayed with distilled water). Potato plants were treated with biostimulators three times (beginning of flowering, full flowering and after plant flowering). Within the presented research the applied biostimulators increased the content of selected mineral components in the tubers of tested varieties. Tubers of plants treated with BrunatneBio Złoto preparation were characterized by the largest content of phosphorus, calcium and magnesium in comparison to the plants from control object. The content of microelements in the tubers varied significantly depending on the genotype of the variety. The greatest concentration of phosphorus was noted in the tubers of Tajfun variety, while in case of magnesium - Honorata variety. Large amount of rainfall in 2017 contributed to the occurrence of an increase of the content of phos.
Tytuł pracy:
Charakterystyka formalna:
Charakterystyka merytoryczna:
Język publikacji:
Praca recenzowana
Słowa kluczowe ang.: ;
Projekt/grant:

10/10
Autorzy: , .
Tytuł całości: W:
ISBN:
Charakterystyka formalna:
Charakterystyka wg MNiSW:
Słowa kluczowe ang.:
Inne bazy podające opis:
  • sustainable Agriculture^bX International Scientific Symposium FMPMSA 2019^ced. by Edmund Lorencowicz, Jacek Uziak, Bruno Huyghebaert^aS. 317-320^aLublin^bInstytut Naukowo-Wydawniczy "Spatium"^c2019^a978-83-66017-74-0^a2019/2020^a10.24362/fmpmsa.2019.1^aŻukiewicz-Sobczak, Wioletta^cy^acereal bran^aKopia dostępna w Sekcji Bibliometrii.^aX International Scientific Symposium FMPMSA 2019^aLublin^dPL^b2019.11.20^c2019.11.22^aBran is a product made of non-waste milling of cereals. Sustainable development in the field of new technologies is increasingly used in food production. Raw materials and cereals are a natural source of fibre, several vitamins (mainly from B, C and E groups) as well as macro and micro elements crucial for maintaining correct body functions. Depending on the content of specific elements they possess uniquely precious properties which may be a determinant of their further use in practice. The objective of this work was to define usefulness of the selected ecological cereal brans on the basis of the conducted mineral analysis CP OES. The following macro elements have been marked and interpreted: Calcium (Ca), Phosphorus (P), Potassium (K), Magnesium (Mg), Sodium (Na), as well as microelements, that is: Cobalt (Co), Chromium (Cr), Copper (Cu), Iron (Fe), Manganese (Mn), Selenium (Se) Zinc (Zn). Furthermore, attention was paid to harmful elements occurring in alarming volumes, such as: Nickel (Ni), Lead (Pb), Aluminium (Al), whilst others, such as: Cadmium (Cd), Arsenic (As), which were located below the limit of quantification.^aRogóż-Matyszczak, Anna^cx^asustainability^aTokarski, Daniel^cx^aelemental analysis^aWeiner, Marcin^cx


      Wyświetl ponownie stosując format:
    • Wyświetl/ukryj etykiety | Wyświetlenie wyników w wersji do druku | Pobranie pliku do edytora | Nowe wyszukiwanie | Biblioteka AB