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Wyświetlanie 1-15 z 119
Tytuł:
The Role of Organic Matter in Tropical Soil Productivity
Autorzy:
Adiaha, M. S.
Powiązania:
https://bibliotekanauki.pl/articles/1178311.pdf
Data publikacji:
2017
Wydawca:
Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
Tematy:
Food security
Human urine
Organic matter
Soil fertility
Tropical soils
Opis:
A survey on the role of soil organic matter (SOM) in tropical soil productivity was carried out with the objective of highlighting on the effects and benefits of organic matter on soil biophysical chemical properties and yield of crops in the tropics. It was revealed that tropical soils are inherently low in fertility due to predominance of kaolinitic clays. The soils are low in CEC, OM, available P and base saturation. Inorganic fertilizers are scarce and costly in addition to negative effects on soil causing acidification and induced micronutrients deficiencies. Organic matter contain a wide range of macro and micro nutrients. On mineralization, these nutrients are released, in addition to contributing of organic matter to the soil. This manure also improves physical properties and ultimately increase crop yield on a sustainable basis.
Źródło:
World Scientific News; 2017, 86, 1; 1-66
2392-2192
Pojawia się w:
World Scientific News
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Hydrophysical properties of Humic Latosols from Brazil
Autorzy:
Ajayi, A.E.
Dias,Jr., M.S.
Curi, N.
Pais, P.S.-M.
Iori, P.
Powiązania:
https://bibliotekanauki.pl/articles/25530.pdf
Data publikacji:
2014
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
organic matter
hydrophysical property
latosol soil
precompression stress
Brazil
Opis:
The hydrophysical properties of the prevalent Humic Latosols (organic matter rich and charcoal stained soils) were related to structural sustainability under loading. Intact cores collected at the Ap, AB, Bw horizons were used for hydrophysical characterization. Precompression stresses at 10 suctions were obtained to estimate the load bearing capacities. We observed the dominance of kaolinite with some occurrences of gibbsite and hydroxy-interlayered vermiculite in the clay mineralogy. The high organic matter content in the Ap horizon favours crumb structure with the structural unit presenting high porosity and water retention. The structure of the AB and Bw horizons was, however, granular with structural units having low porosity. Possible influence of earlier incidences of fire enhanced the organic matter and carbon content in the soil reducing down the profile from 42.5 g kg-1 at the Ap to 16.4 g kg-1 at the Bw horizon. The C/N ratio increased from 14 at the Ap to 17 at the Bw, and air capacity increased from 18.1% at Ap to 32.0% at Bw. Precompression stress values were: 100.6±40.7 kPa at Ap, 117.4±44.6 kPa at AB, and 116.1±58.9 kPa at Bw. Load bearing capacities at the AB and Bw horizons were homogenous.
Źródło:
International Agrophysics; 2014, 28, 4
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The structural state of soils on loesses
Autorzy:
Alekseeva, T.
Alekseev, A.
Morgun, Y.
Jozefaciuk, G.
Powiązania:
https://bibliotekanauki.pl/articles/25999.pdf
Data publikacji:
1995
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
mineral soil compound
soil structure
soil profile
organic matter composition
organic soil compound
aggregation
soil
loess
soil aggregate
Źródło:
International Agrophysics; 1995, 09, 3
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Impact of short- and long-term agricultural use of chernozem on its quality indicators
Autorzy:
Balashov, E.
Buchkina, N.
Powiązania:
https://bibliotekanauki.pl/articles/24527.pdf
Data publikacji:
2011
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
short-term use
long-term use
agricultural use
black earth
quality indicator
soil use
soil quality
organic matter
thermodynamics
Źródło:
International Agrophysics; 2011, 25, 1
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Dynamics of organic matter in peat soil under the conditions of sand-mix culture during 15 years
Autorzy:
Bambalov, N.
Powiązania:
https://bibliotekanauki.pl/articles/24852.pdf
Data publikacji:
1999
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
organic matter
peat soil
soil
sand-mix culture
dynamics
Źródło:
International Agrophysics; 1999, 13, 2
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Soil colour and spectral analysis employing linear regression models. I. Effect of organic matter
Autorzy:
Barouchas, P.E.
Moustakas, N.K.
Powiązania:
https://bibliotekanauki.pl/articles/26488.pdf
Data publikacji:
2004
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
organic matter
soil colour
spectral analysis
soil property
colour
Źródło:
International Agrophysics; 2004, 18, 1
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Morphology and properties of permafrost-affected soils under different tundra vegetation in central Spitsbergen
Autorzy:
Bartos, Anna
Szymański, Wojciech
Gus-Stolarczyk, Magdalena
Powiązania:
https://bibliotekanauki.pl/articles/16648057.pdf
Data publikacji:
2023
Wydawca:
Polska Akademia Nauk. Czasopisma i Monografie PAN
Tematy:
Arctic
Svalbard
soil organic matter
heath and pioneer tundra
Cryosols
Opis:
The main aim of this study was to determine the morphology, physical and chemical properties of permafrost-affected soils under different types of tundra in the central part of Spitsbergen. This is a preliminary part of detailed studies focused on the relationship between tundra vegetation and permafrost-affected soils in the Spitsbergen. The obtained results indicate that all the studied soils represent an early stage of formation and the main soil-forming process present in these soils is cryoturbation. Most of the studied soils are shallow and contain a high content of coarse rock fragments. Tundra vegetation type plays controlling role in the development and structure of surface soil horizons. All the studied soils are characterized by loamy texture and acidic or slightly acidic reaction, and these properties are not very different under various tundra vegetation types. The contents of soil organic matter are strongly dependent on the type of tundra vegetation. The highest soil organic matter content occurs at sites with well-developed vegetation such as heath and wet moss tundra. The high carbon-to-nitrogen ratio for the surface soil horizons of the majority of the studied soils indicates that organic matter is poorly decomposed under all the studied tundra vegetation types. This is most likely related to low activity of soil microorganisms in the harsh High Arctic environment. However, the lowest carbon-to-nitrogen ratio was noted for surface soil horizons at sites covered with Arctic meadow, and this indicates that there occur the optimum conditions for soil organic matter decomposition.
Źródło:
Polish Polar Research; 2023, 44, 1; 1-20
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Charakterystyka i zmiany jakościowe materii organicznej gleb w wyniku zalewu woda w doświadczeniu lizymetrycznym
The properties and qualitative changes of soil organic matter after flooding in a lysimetric experiment
Autorzy:
Becher, M.
Kalembasa, D.
Pakuła, K.
Powiązania:
https://bibliotekanauki.pl/articles/338783.pdf
Data publikacji:
2008
Wydawca:
Instytut Technologiczno-Przyrodniczy
Tematy:
doświadczenie lizymetryczne
frakcje glebowej materii organicznej
lysimetric experiment
soil organic matter fractions
Opis:
W pracy przedstawiono wyniki badań jakości materii organicznej poziomów próchnicznych mady i hortisolu (pobranych z dolin rzecznych Muchawki i Liwca) oraz jej zmian pod wpływem zalewania gleb wodą w lizymetrach (na okres 10 i 25 dni). Frakcjonowanie materii organicznej przeprowadzono metodą Shnitzera. W pracy podano zawartość węgla i azotu we frakcjach kwasów huminowych i fulwowych (wyekstrahowane za pomocą roztworu NaOH) i w poekstrakcyjnej pozostałości oraz stosunek węgla kwasów huminowych do węgla kwasów fulwowych. Zmierzono absorbancję w zakresie światła widzialnego przez roztwór kwasów huminowych i obliczono stosunek absorbancji A465 do A665 (A4/6). W obydwu glebach zalanych wodą istotnie zwiększyła się ilość węgla i azotu należącego do frakcji kwasów huminowych i fulwowych oraz zmniejszyła się ilość tych pierwiastków w poekstrakcyjnej pozostałości; nieznacznie wzrosła wartość stosunku węgla kwasów huminowych do węgla kwasów fulwowych oraz iloraz wartości A4/6 kwasów huminowych. Zmiany dotyczyły głównie 10-dniowego okresu zalania gleb wodą.
This paper presents results of soil organic matter analyses of Fluvisol and Hotric Anthrosol humic horisons from the Muchawka and Liwiec river valleys flooded in lysimeters for 10 and 25 days. Organic matter was fractionated with the Shnitzer method. The content of carbon and nitrogen in humic acids, fulvic acids, and residual fraction and the ratio of humic to fulvic acids are given in this paper. Visible light absorbance by humic acids was measured spectrophotometrically and the ratio of A465 to A665 (A4/6) was calculated. Carbon and nitrogen content in humic and fulvic acid fractions significantly increased in both soils after flooding. The content of the two elements decreased in post-extraction residuals. The ratio of humic to fulvic acids carbon slightly increased as did the A4/6 ratio of humic acids. These changes pertained mainly to the 10-days long flooding period.
Źródło:
Woda-Środowisko-Obszary Wiejskie; 2008, T. 8, z. 2a; 5-12
1642-8145
Pojawia się w:
Woda-Środowisko-Obszary Wiejskie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Biochar usefulness in achieving goals of carbon farming and sustainable agricultural systems
Autorzy:
Berbeć, Adam Kleofas
Wyzińska, Marta
Berbeć, Tytus
Powiązania:
https://bibliotekanauki.pl/articles/37244720.pdf
Data publikacji:
2023
Wydawca:
Instytut Uprawy Nawożenia i Gleboznawstwa – Państwowy Instytut Badawczy
Tematy:
biochar
sustainable agriculture
soil organic matter
carbon farming
Opis:
This paper presents an overview of the literature research on the benefits of biocarbon (biochar) as an important part of sustainable agriculture and carbon farming. The main objective was to familiarise the reader with the literature findings on the effects of biocarbon application on the environment, soil, soil organic mater, soil microorganisms, and impact on crop yields. On the basis of the research presented, it can be concluded that the incorporation of biocarbon into the soil generally has a positive effect on soil fertility, but that proper application is required (mainly its application together with fertilization). The quality, properties, and agricultural usefulness of the biochar depend on the raw material that has been subjected to the pyrolysis process, as well as the temperature and time of. The findings of the paper are based on the literature review on the subject.
Źródło:
Polish Journal of Agronomy; 2023, 52; 145-156
2081-2787
Pojawia się w:
Polish Journal of Agronomy
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Rate of humus accumulation on anthropic protosol from the Capus-Cluj District
Autorzy:
Blaga, G
Bunescu, V.
Rauta, C.
Dumitru, M.
Lacatusu, R.
Vidican, R.
Lechintan, T.
Gamet, E.
Clapa, D.
Powiązania:
https://bibliotekanauki.pl/articles/1450112.pdf
Data publikacji:
2001
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
organic matter
surface mining
rock type
accumulation
deposit exploitation
climate
recultivation
soil
humus
soil property
Capos-Cluj District
degraded ecosystem
anthropogenic ecosystem
relief condition
Opis:
The paper presents data on the annual rate of humus accumulation after 10 and 20 years of a strict experimental routine carried out on sterile waste dumps (anthropic protosol) from Cápuş, cultivated with maize, oat and esparcet. Basic dressing applied was the following: V1 - unfertilized, V2- 40 t/ha manure, V3 - 15 t/ha poultry manure, V4 - 40 t/ha manure + N100 P60 K40 , V5 - 15 t/ha poultry manure + N100 P60 K40 , V6 - N100 P60 K0 , V7 - N100 P60 K40, V8 - N200 P120 K80 , V9 - N300 P180 K120. The results obtained revealed that the variant with 40 t/ha manure + N100 P6O K40 (V4) after 10 years accumulated 1.724% humus and after 20 years 4.100% humus. It means that the annual average rate was 0.115% and 0.176%, respectively, at a depth of 0-20 cm. The next variant is the variant with 15 t/ha poultry manure + N100 P60 K40 (V5) where 1.207% of humus was accumulated after 10 years and 3.760% of humus after 20 years; the annual average rate 0.055% and 0.155%, respectively.
Źródło:
Acta Agrophysica; 2001, 51; 15-19
1234-4125
Pojawia się w:
Acta Agrophysica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Characteristics of the meadow hydrogenic soils in Przedmoscie against the background of forming plant communities
Autorzy:
Bogacz, A
Grosdzinska, D.
Chachula, K.
Kasowska, D.
Powiązania:
https://bibliotekanauki.pl/articles/1450407.pdf
Data publikacji:
2001
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
organic matter
physicochemical property
physical property
hydrogenic soil
chemical property
plant community
soil
meadow soil
soil property
melioration
terrestrial ecosystem
Opis:
The aim of this work was to compile characteristics of some selected physical, physico-chemical and chemical properties of the reclaimed hydrogenic soils in the meadow part of the Przedmoście bog in the context of new forming plant communities. Melioration work conducted in this area before the Second World War ended peat accumulation processes. Consequently, drying peat began to disintegrate and mineralise. Analyses of floral lists proved that the existing vegetation replaced the original bog plant communities, which flourished in this area in the past. Descriptions of profiles point to the existence of mixed formations (gyttja, peat) often containing high quantities of CaCO3. Peat formations present in the profiles are usually at the advanced degree of decomposition (H>7) and contain substantial quantities of ash. This high degree of ash content and bulk density results in strong compaction and muddy soil horizons. A low coefficient of C/N showed intense mineralization of organic matter in the upper soil horizons.
Źródło:
Acta Agrophysica; 2001, 50; 17-28
1234-4125
Pojawia się w:
Acta Agrophysica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Loss-on-ignition as an estimate of total organic carbon in the mountain soils
Straty prażenia jako podstawa wyliczania całkowitej zawartości węgla organicznego w glebach górskich
Autorzy:
Bojko, O.
Kabala, C.
Powiązania:
https://bibliotekanauki.pl/articles/905700.pdf
Data publikacji:
2014
Wydawca:
Uniwersytet Marii Curie-Skłodowskiej. Wydawnictwo Uniwersytetu Marii Curie-Skłodowskiej
Tematy:
total organic carbon
carbon
soil organic matter
determination
soil
mountain soil
Opis:
Due to the ease and low cost of implementation, a commonly used method of determining the humus content in soils is the loss-on-ignition (LOI) method. Several regression equations and transformation factors are reported for LOI conversion to soil organic matter (SOM) or total organic carbon (TOC) content. The vast majority of the conversion factors have been developed for surface horizons of lowland soils, while there are only few findings from the mountainous areas. 476 mineral and 79 organic (forest litter) samples from 31 soil profiles located in different altitude zones of the Karkonosze Mountains and under different vegetation were used for analysis. LOI was determined by the drying-weighing method and TOC by the dry combustion method with CO₂ absorption. The average LOI/TOC ratio was about 2, but varied in accordance to LOI value. At the LOI value above 8–10%, the LOI/TOC is maintained at a constant level of 2.0, but with a decreasing LOI it may significantly extend, up to 20 at LOI <1%. In the mountain soils, the best compatibility of TOC determined and estimated based on LOI was obtained when using different conversion factors ( 7.3, 5.0, 3.1 and 2.0) for the four LOI ranges (0–2, 2–4, 4–8, and > 8%, respectively) or when using separate regression equations for LOI of <8 and >8%. Because of huge TOC overestimation by LOI method at LOI values lower than 8–10%, the conversion LOI to TOC is not recommended, unless the direct measurement of TOC content is currently unavailable (e.g. in archival databases).1
Źródło:
Polish Journal of Soil Science; 2014, 47, 2
0079-2985
Pojawia się w:
Polish Journal of Soil Science
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geospatial Assessment of Soil Organic Matter Variability at Sidi Bennour District in Doukkala Plain in Morocco
Autorzy:
Bouasria, Abdelkrim
Ibno Namr, Khalid
Rahimi, Abdelmejid
Ettachfini, El Mostafa
Powiązania:
https://bibliotekanauki.pl/articles/2028049.pdf
Data publikacji:
2021
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
soil organic matter
Doukkala Plain
spatial interpolation
geostatistics
soil quality
irrigated perimeter
Morocco
Opis:
Understanding the spatial variability of soil organic matter (SOM) is critical for studying and assessing soil fertility and quality. This knowledge is important for soil management, which results in high crop yields at a reduced cost of crop production and helps to protect the environment. The benefits of an accurate interpolation of SOM spatial distribution are well known at the agricultural, economic, and ecological levels. It has been conducted this study for comparing and analyze different spatial interpolation methods to evaluate the spatial distribution of SOM in Sidi Bennour District, which is a semi-arid area in the irrigated scheme of the Doukkala Plain, Morocco. For conding this study, it was collected 368 representative soil samples at a depth of 0–30 cm. A portable global positioning system was used to obtain the location coordinates of soil sampling sites. The SOM spatial distribution was performed using four interpolation methods: inverse distance weighted and local polynomial interpolation as deterministic methods, and ordinary kriging and empirical Bayesian kriging as geostatistical methods. High SOM levels were concentrated in vertisols, and low SOM levels were observed in immature soils. The average SOM value was 1.346%, with moderate to high variability (CV = 35.720%). A low SOM concentration indicates a continuous possibility of soil degradation in the future. Ordinary kriging yielded better results than the other interpolation methods (RMSE = 0.395) with a semivariogram fitted by an exponential model, followed by inverse distance weighted (RMSE = 0.397), empirical Bayesian kriging (RMSE = 0.400), and local polynomial interpolation (RMSE = 0.412). Soil genetics and the strong influence of human activity are the major sources of SOM spatial dependence, which is moderate to low. Low SOM content levels (< 1.15%) were present in the southwestern and eastern parts of the digital map. This situation calls for the implementation of specific soil recovery measures.
Źródło:
Journal of Ecological Engineering; 2021, 22, 11; 120-130
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Impact of agricultural use on chosen soil properties
Autorzy:
Braun, Barbara
Powiązania:
https://bibliotekanauki.pl/articles/2029783.pdf
Data publikacji:
2008-06-01
Wydawca:
Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
Tematy:
agricultural use
soil reaction
bulk density
organic matter
Opis:
Agricultural use may change soil. These changes may be observed by examining certain soil properties. In numerous cases of agricultural use, soil compaction may be observed at the depth of 25-35 cm. After many years of use, this may lead to the creation of a plough sole. On arable grounds, which are generally fertilized by minerals, a decrease in organic matter content and soil acidification are frequently observed. Each human activity leads to changes in the natural environment. In the case of agricultural use, the greatest changes take place in soil. Mechanization in agriculture and the wish to produce ever-greater amounts of crops influence changes in some soil properties. In a short time, changes in soil reaction, organic matter content or creation of a plough sole at the depth of 25-35 cm may observed.
Źródło:
Miscellanea Geographica. Regional Studies on Development; 2008, 13; 153-162
0867-6046
2084-6118
Pojawia się w:
Miscellanea Geographica. Regional Studies on Development
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Rozmieszczenie materii organicznej i azotu we frakcjach granulometrycznych poziomów genetycznych gleby brunatnej wyługowanej Lasu Kabackiego
Distribution of organic matter and nitrogen in the particle size fractions of genetic horizons in Dystric Cambisols in the Kabacki Forest
Autorzy:
Brogowski, Z.
Chojnicki, J.
Powiązania:
https://bibliotekanauki.pl/articles/991709.pdf
Data publikacji:
2013
Wydawca:
Polskie Towarzystwo Leśne
Tematy:
gleboznawstwo lesne
gleby brunatne wylugowane
poziomy glebowe
frakcje granulometryczne
materia organiczna
zawartosc materii organicznej
azot
zawartosc azotu
stosunek wegla do azotu
Las Kabacki
soil organic matter
nitrogen
granulometric fractions
Opis:
Organic matter and nitrogen content was analysed in genetic horizons of Dystric Cambisols in the Kabacki Forest (Warsaw, central Poland). Particle size fractions in investigated soil indicated the following contribution in binding of organic matter: 0.1−0.02 mm – 7.6%, 0.02−0.01 mm – 13.2%, 0.01−0.005 mm – 18.8%, 0.005−0.002 mm – 21.9% and <0.002 mm – 37.8%. Sand fractions with 1−0.1 mm particles accumulate only 0.7% of the total organic matter content. Nitrogen showed similar distribution among the particular fractions. Horizons A and ABbr to the depth of 25 cm accumulate 75.8% organic matter, horizons located at the depth of 25−100 cm − 14.6%, whereas the parent rock lying at 100−125 cm on poorly permeable glacial till gathers 9,9% of the total organic matter accumulated in the entire profile. The leaching pedogenetic process and the particle size diameter significantly influenced the translocation of organic matter and nitrogen in the studied soil profile.
Źródło:
Sylwan; 2013, 157, 06; 470-480
0039-7660
Pojawia się w:
Sylwan
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 119

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