Fluctuations in the properties of forest soils in the Central European highlands (Czech Republic)
Fluctuations in forest soil properties were described using a time series analysis of the clay content, the chemical (CaO, MgO, Corg, and Ntot) and physicochemical (pH and base saturation (BS)) soil parameters from 1953 to 2008. The analysis involved the dominant acidic, nutrient-rich, and waterlogged forest ecosystems on the territory of the Bohemian Massif … celý popis
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- Soil and Water Research. -- ISSN 1801-5395. -- Roč. 9, č. 4 (2014), s. 201-213
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- 16 grafů, 3 tabulky
- Bibliografie
- Seznam literatury na s. 211-213,
MARC
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| 072 | 7 | |a 630 |x Lesnictví |2 Konspekt |9 24 | |
| 072 | 7 | |a 556 |x Hydrologie |2 Konspekt |9 7 | |
| 072 | 7 | |a 631 |x Zemědělství. Pedologie. Agrotechnika. Agroekologie |2 Konspekt |9 24 | |
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| 100 | 1 | |a Samec, Pavel, |d 1979- |u Univerzita Palackého, Přírodovědecká fakulta, Katedra geoinformatiky, Olomouc ; Ústav hospodářské úpravy lesů, Brandýs nad Labem |7 mzk2006320210 |4 aut | |
| 245 | 1 | 0 | |a Fluctuations in the properties of forest soils in the Central European highlands (Czech Republic) / |c Pavel Samec, Aleš Kučera, Pavel Tuček |
| 300 | |b 19 il. | ||
| 500 | |a 16 grafů, 3 tabulky | ||
| 504 | |a Seznam literatury na s. 211-213, |b 43 záznamů | ||
| 520 | 3 | 9 | |a Fluctuations in forest soil properties were described using a time series analysis of the clay content, the chemical (CaO, MgO, Corg, and Ntot) and physicochemical (pH and base saturation (BS)) soil parameters from 1953 to 2008. The analysis involved the dominant acidic, nutrient-rich, and waterlogged forest ecosystems on the territory of the Bohemian Massif and the Outer Western Carpathians (Czech Republic). Trends in the development of the time series of soil properties were optimized by Gauss-Newton’s transformation of the exponential combination of the cyclometric function and Euler’s number. Identical functions of regression equations on the fluctuations of nutrients, pH, BS, and Corg indicated parallel trends of soil development in different forest ecosystems. Equations representing identical, predictable patterns in Corg fluctuation indicated the stability of the trend. Differences in temporal patterns of nutrients, pH, and BS in different forest ecosystems indicated the susceptibility of developmental trends to external factors. Different regression equations of fluctuations of soil clay and Ntot indicated the occurrence of permanent differences during the soil development. During the period of 1953-2008, soil pH, BS, and CaO concentration decreased but the content of Corg and Ntot increased. Regression functions indicate that pH and BS of forest soils in the Czech Republic have temporarily increased and the content of Corg and Ntot have decreased during the period 2009-2014. Continuous increase in BS is only sustainable if concurrent with an increase in Corg. |9 eng |
| 530 | |a Dostupné též na internetu | ||
| 546 | |a Anglický text, anglický abstrakt | ||
| 650 | 0 | 9 | |a CZECH REPUBLIC |
| 650 | 0 | 9 | |a TEMPERATE FORESTS |
| 650 | 0 | 9 | |a state forests |
| 650 | 0 | 9 | |a HIGHLANDS |
| 650 | 0 | 9 | |a ECOSYSTEMS |
| 650 | 0 | 9 | |a SURVEYS |
| 650 | 0 | 9 | |a CLASSIFICATION |
| 650 | 0 | 9 | |a PLANT COMMUNITIES |
| 650 | 0 | 9 | |a INDICATOR PLANTS |
| 650 | 0 | 9 | |a SPATIAL DISTRIBUTION |
| 650 | 0 | 9 | |a Tree and stand measurement |
| 650 | 0 | 9 | |a FOREST SURVEYS |
| 650 | 0 | 9 | |a WATERLOGGING |
| 650 | 0 | 9 | |a WATERSHEDS |
| 650 | 0 | 9 | |a FOREST MANAGEMENT |
| 650 | 0 | 9 | |a FOREST SOILS |
| 650 | 0 | 9 | |a SOIL DEGRADATION |
| 650 | 0 | 9 | |a anthropogenic factors |
| 650 | 0 | 9 | |a ACIDIFICATION |
| 650 | 0 | 9 | |a nutrient cycling in ecosystems |
| 650 | 0 | 9 | |a SOIL TYPES |
| 650 | 0 | 9 | |a SOIL CHEMICOPHYSICAL PROPERTIES |
| 650 | 0 | 9 | |a SOIL PH |
| 650 | 0 | 9 | |a ION EXCHANGE CAPACITY |
| 650 | 0 | 9 | |a Organic matter content |
| 650 | 0 | 9 | |a CALCIUM OXIDE |
| 650 | 0 | 9 | |a NITROGEN CONTENT |
| 650 | 0 | 9 | |a SIMULATION MODELS |
| 650 | 0 | 9 | |a TIME SERIES ANALYSIS |
| 650 | 0 | 9 | |a STATISTICAL DATA |
| 650 | 0 | 7 | |a lesy mírného pásma |2 agrovoc |
| 650 | 0 | 7 | |a státní lesy |2 agrovoc |
| 650 | 0 | 7 | |a vyšší polohy |2 agrovoc |
| 650 | 0 | 7 | |a ekosystémy |2 agrovoc |
| 650 | 0 | 7 | |a průzkumy |2 agrovoc |
| 650 | 0 | 7 | |a klasifikace |2 agrovoc |
| 650 | 0 | 7 | |a rostlinná společenstva |2 agrovoc |
| 650 | 0 | 7 | |a indikátorové rostliny |2 agrovoc |
| 650 | 0 | 7 | |a prostorové rozšíření |2 agrovoc |
| 650 | 0 | 7 | |a měření stromů a porostů |2 agrovoc |
| 650 | 0 | 7 | |a inventarizace lesů |2 agrovoc |
| 650 | 0 | 7 | |a zamokření |2 agrovoc |
| 650 | 0 | 7 | |a povodí |2 agrovoc |
| 650 | 0 | 7 | |a lesní hospodářství |2 agrovoc |
| 650 | 0 | 7 | |a lesní půdy |2 agrovoc |
| 650 | 0 | 7 | |a znehodnocování půdy |2 agrovoc |
| 650 | 0 | 7 | |a antropogenní faktory |2 agrovoc |
| 650 | 0 | 7 | |a acidifikace |7 ph622011 |2 czenas |
| 650 | 0 | 7 | |a koloběh živin |2 agrovoc |
| 650 | 0 | 7 | |a půdní typy |2 agrovoc |
| 650 | 0 | 7 | |a chemickofyzikální půdní vlastnosti |2 agrovoc |
| 650 | 0 | 7 | |a půdní pH |2 agrovoc |
| 650 | 0 | 7 | |a výměnná iontová kapacita |2 agrovoc |
| 650 | 0 | 7 | |a obsah organické hmoty |2 agrovoc |
| 650 | 0 | 7 | |a oxid vápenatý |2 agrovoc |
| 650 | 0 | 7 | |a obsah dusíku |2 agrovoc |
| 650 | 0 | 7 | |a simulační modely |2 agrovoc |
| 650 | 0 | 7 | |a analýza časových řad |2 agrovoc |
| 650 | 0 | 7 | |a statistické údaje |2 agrovoc |
| 651 | 7 | |a Česko |7 ge128065 |2 czenas | |
| 700 | 1 | |a Kučera, Aleš |u Mendelova univerzita v Brně, Lesnická a dřevařská fakulta, Ústav geologie a pedologie |7 mzk2015860566 |4 aut | |
| 700 | 1 | |a Tuček, Pavel, |d 1980- |u Univerzita Palackého, Přírodovědecká fakulta, Katedra geoinformatiky, Olomouc |7 jo2013741795 |4 aut | |
| 773 | 0 | |t Soil and Water Research |x 1801-5395 |g Roč. 9, č. 4 (2014), s. 201-213 |q 9:4 |9 2014 | |
| 856 | 4 | 1 | |u https://www.agriculturejournals.cz/publicFiles/136474.pdf |q text/pdf |y Plný text |4 N |
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| 990 | |a RS | ||
| 998 | |a http://aleph.nkp.cz/F/?func=direct&doc_number=001547976&local_base=ANL | ||