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Wyszukujesz frazę "soil water conductivity" wg kryterium: Temat


Tytuł:
Impact of wood-derived biochar on the hydraulic characteristics of compacted soils: Its influence on simulated farmland carbon sequestration
Autorzy:
Ahmed, A.
Kurian, J.
Satyanarayana, S.
Raghavan, V.
Powiązania:
https://bibliotekanauki.pl/articles/2083067.pdf
Data publikacji:
2021
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
soil biochar mixture
water retention
pore-size
distribution
hydraulic conductivity
carbon sequestration
Opis:
The addition of biochar is often proposed to increase agricultural soil quality and crop yield, while at the same time sequestering carbon from the atmosphere to help mitigate global climate change. In this research, the pore-size distribution, and saturated hydraulic conductivity of sandy loam and clay loam soils amended with varying dosages (0-10% dry basis) and two different particle sizes (0.5-420 μm (PS1) or 421-841 μm (PS2)) of wood-derived biochar were investigated under compacted conditions (5, 10, or 15 standard Proctor rammer blows (5B, 10B, or 15B, respectively)). In the 5B compacted SL (SL-5B) soil, the volume of the soil fissures and transmission pores decreased, while the volume of the storage pores (SP) increased with increasing wood-derived biochar dosage. 23.1±0.9% of the volume of the 5B compacted clay loam (CL-5B) are storage pores, this value increased to 27.4±2.0% upon amendment with 10% PS1. The saturated hydraulic conductivity of the sandy loam-5B soil amended with 10% PS1 decreased from 6.8±0.3 to 0.80±0.03 mm h-1. The sandy loam farmland C emissions decreased by 0.071 tC ha-1 y-1, whereas CL farmland C emissions decreased by 0.091 tC ha-1 y-1.
Źródło:
International Agrophysics; 2021, 35, 2; 167-177
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Impact of marble powder amendment on hydraulic properties of a sandy soil
Autorzy:
Farhadi-Machekposhti, M.
Valdes-Abellan, J.
Pla, C.
Benavente, D.
Pachepsky, Y.
Powiązania:
https://bibliotekanauki.pl/articles/2082885.pdf
Data publikacji:
2020
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
saturated hydraulic conductivity
soil water
retention curve
field capacity
plant available water
pore size
distribution
Opis:
Marble powder is one of carbonate rock amendments that is used to improve soil reaction. We hypothesized that the powdered marble addition can cause favorable changes in hydraulic properties of sandy soils. Six levels of marble powder addition to an aridisol soil (0%; M0; 5%; M5; 10%; M10; 15%; M15; 20%; M20 and 25%, M25; by bulk volume) were analyzed in triplicate. The saturated hydraulic conductivity and soil water retention curves were obtained. Pore space properties were investigated using soil water retention curves, mercury intrusion porosimetry and scanning electron microscopy. The saturated hydraulic conductivity significantly decreased (between 83 and 97% for M5 and M25 respectively) and parameters α and n of the van Genuchten model significantly decreased in marble-amended soils. Both field capacity and permanent wilting point increased with the addition of marble powder. Plant-available water, increased significantly until 10% of marble powder application; higher percentages of application did not provide additional significant changes in the plant-available water. Pore space distributions from soil water retention curves parameters showed an increase in the pore size range and a decrease in the average pore size; pore space distribution from the scanning electron microscopy also showed the presence of a new family of dominant pore sizes which was not detected by the soil water retention curves parameters approach. It was concluded that the addition of marble powder can improve the ability of soil to store water providing an advantage for irrigation water management in water scarce environments. Further research will have to address the impact of marble powder amendment under field semi-arid conditions.
Źródło:
International Agrophysics; 2020, 34, 2; 223-232
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New pedotransfer function (“CRC”) for the prediction of unsaturated soil hydraulic conductivity using soil water retention data
Autorzy:
Bohne, K.
Renger, M.
Wessolek, G.
Powiązania:
https://bibliotekanauki.pl/articles/2082651.pdf
Data publikacji:
2019
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
soil texture
hydraulic conductivity
transfer
function
soil water retention
Opis:
Several review articles have emphasized, that a comprehensive set of pedotransfer functions may be applied throughout a wide range of disciplines of Earth system sciences and are of great importance for land surface models. Most pedotransfer functions deducing soil hydraulic data from nonhydraulic soil data such as soil texture and bulk density, yield soil water retention predictions, but do not provide information concerning soil hydraulic conductivity. For this reason, a simple method was developed to estimate soil hydraulic conductivity using soil water retention information. Empirical equations are established to predict soil hydraulic conductivity from soil water retention information. These equations are relatively straightforward and do not require the fitting of nonlinear functions. Predictions of soil hydraulic conductivity using 106 soil samples indicates the reliable performance of the new method. The prediction quality of the new method was estimated from the calibration data set, which produced equivalent results to the Zacharias and Wessolek pedotransfer function, which were even better than the predictions obtained from the original Mualem-van Genuchten model, the Soto fractal model, and the pedotransfer function reported by Weynants and Vereecken. The stochastic structure of the calibration data reflects the presence of important soil structural properties, which are not represented by the soil water retention characteristics.
Źródło:
International Agrophysics; 2019, 33, 4; 503-510
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Temporal stability of electrical conductivity in a sandy soil
Autorzy:
Pedrera-Parrilla, A.
Brevik, E.C.
Giraldez, J.V.
Vanderlinden, K.
Powiązania:
https://bibliotekanauki.pl/articles/26163.pdf
Data publikacji:
2016
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
temporal stability
electrical conductivity
sandy soil
soil texture
soil water content
spatial variability
Źródło:
International Agrophysics; 2016, 30, 3
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Scaling the hydraulic functions of a water repellent sandy soil
Autorzy:
Stoffregen, H.
Wessolek, G.
Powiązania:
https://bibliotekanauki.pl/articles/24417.pdf
Data publikacji:
2014
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
scaling
hydraulic function
hydraulic conductivity
water retention
hysteresis
water repellent
sandy soil
Opis:
The heterogeneity of both unsaturated hydraulic conductivity and water retention was measured with a high spatial resolution on a transect using an evaporation method. Fifteen undisturbed 100 cm 3 soil cores were taken on a transect every 10 cm from the topsoil of a water repellent sandy site. Five dynamic water retention curves and four unsaturated conductivity curves were determined for each core. We conducted measurements without further saturation in the laboratory in order to achieve field-like conditions. The initial water contents were hetero- geneous, indicating different hysteretic conditions and water repellent areas. The scattering of the water retention curves was high, while the heterogeneity of unsaturated conductivity curves was unexpectedly low. Two scaling approaches were used to describe the heterogeneity: one with and one without considering hysteresis. The concept of scaling applies well to describing the heterogeneity of both hydraulic functions. Including hysteresis leads to similar results than excluding hysteresis. The distribution of the hydraulic conductivity and the water retention were inde- pendent from each other. The results give important information for numerical simulation of the water flow with heterogeneous hydraulic functions.
Źródło:
International Agrophysics; 2014, 28, 3
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Water conductivity of Arctic zone soils (Spitsbergen)
Autorzy:
Witkowska-Walczak, B.
Slawinski, C.
Bartminski, P.
Melke, J.
Cymerman, J.
Powiązania:
https://bibliotekanauki.pl/articles/25209.pdf
Data publikacji:
2014
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
water conductivity
soil
grain size
distribution
pore size
Arctic zone
Spitsbergen
Opis:
The water conductivity of arctic zone soils derived in different micro-relief forms was determined. The greatest water conductivity at the 0-5 cm depth for the higher values of water potentials (> -7 kJ m-3) was shown by tundra polygons (Brunic-Turbic Cryosol, Arenic) – 904-0.09 cm day-1, whereas the lowest were exhibited by Turbic Cryosols – 95-0.05 cm day-1. Between -16 and -100 kJ m-3, the water conductivity for tundra polygons rapidly decreased to 0.0001 cm day-1, whereas their decrease for the other forms was much lower and in consequence the values were 0.007, 0.04, and 0.01 cm day-1 for the mud boils (Turbic Cryosol (Siltic, Skeletic)), cell forms (Turbic Cryosol (Siltic, Skeletic)), and sorted circles (Turbic Cryosol (Skeletic)), respectively. In the 10-15 cm layer, the shape of water conducti-vity curves for the higher values of water potentials is nearly the same as for the upper layer. Similarly, the water conductivity is the highest – 0.2 cm day-1 for tundra polygons. For the lower water potentials, the differences in water conductivity increase to the decrease of soil water potential. At the lowest potential the water conductivity is the highest for sorted circles – 0.02 cm day-1 and the lowest in tundra polygons – 0.00002 cm day-1.
Źródło:
International Agrophysics; 2014, 28, 4
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Error analysis of water conductivity coefficient measurement by instantaneous profiles method
Autorzy:
Slawinski, C.
Walczak, R.T.
Skierucha, W.
Powiązania:
https://bibliotekanauki.pl/articles/26183.pdf
Data publikacji:
2006
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
conductivity coefficient
soil water
instantaneous profiles method
coefficient measurement
water conductivity
error analysis
water potential value
Źródło:
International Agrophysics; 2006, 20, 1
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Recent software improvements in moisture [TDR method], matric pressure, electrical conductivity and temperature meters of porous media
Autorzy:
Skierucha, W.
Wilczek, A.
Walczak, R.T.
Powiązania:
https://bibliotekanauki.pl/articles/24442.pdf
Data publikacji:
2006
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
moisture
electrical conductivity
user interface
temperature
porous medium
soil water
soil salinity
time domain reflectometry
soil temperature
water content
Źródło:
International Agrophysics; 2006, 20, 3
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ocena i kartograficzna prezentacja wrażliwości gleb ornych na hydrooksygeniczną degradację
Evaluation and cartographic presentation of arable soil susceptability to hydrooxygenic degradation
Autorzy:
Ostrowski, J.
Sławiński, C.
Walczak, R.
Powiązania:
https://bibliotekanauki.pl/articles/338591.pdf
Data publikacji:
2004
Wydawca:
Instytut Technologiczno-Przyrodniczy
Tematy:
gleby mineralne
hydrooksygeniczna degradacja
procesy oksydoredukcyjne
przewodnictwo wodne
hydrooxygenic degradation
mineral soils
redox processes
soil water conductivity
Opis:
W pracy omówiono uwarunkowania degradacji gleb mineralnych spowodowane czynnikiem wodnym i przedstawiono możliwość ich sparametryzowania. Na podstawie współzależności między zapełnieniem wodą porów grawitacyjnych, a stanem natlenienia gleby postawiono tezę, że zależy on od odporności oksydoredukcyjnej i zdolności samonatlenienia się gleb przez odpływ z jej profilu wody grawitacyjnej. Stosunek czasu wyrażającego odporność gleb na redukcję (t300) do czasu samonatlenienia się gleby zdefiniowano jako wskaźnik potencjalnej wrażliwości gleb na hydrooksygeniczną degradację.
This paper presents results of a study on chemical and physical properties of soils conducted in cooperation between the Institute of Agrophysics PAS in Lublin and the Institute of Land Reclamation . Basic assumption of these investigations is the hypothesis that the hydro-oxygenic susceptibility can be expressed by the ratio of the time in which redox potential of fully saturated soil decreases to +300 mV (reduction of ferric ions) to the time in which fully saturated soil proceeds to the state of field capacity (outflow of gravitational water). This index can be expressed by the equation: Dho= t300 / TPPW The value of this index was analysed in three soil horizons: surface, subsurface and subsoil (70-110 cm) as diagnostic layers. For evaluation of soil susceptibility the following denotations have been applied: NW - soils unsusceptible to hydro-oxygenic degradation, index Dho ≥ 1 in the whole soil profile, MW - soils slightly susceptible to hydro-oxygenic degradation, index Dho < 1 in only one diagnostic horizon, W - soils susceptible to hydro- oxygenic degradation, index Dho < 1 in two diagnostic horizons, BW - soils very susceptible to hydro-oxygenic degradation, index Dho < 1 in all soil profiles. According to above mentioned principles, systematic investigations of Polish arable mineral soils were conducted. Values of the Dho index were quantified and evaluation of susceptibility to hydro-oxygenic degradation of Polish arable, mineral soils was performed. Results of the study are presented as a spatial characteristics on digital, thematic maps.
Źródło:
Woda-Środowisko-Obszary Wiejskie; 2004, T. 4, z. 2a; 185-200
1642-8145
Pojawia się w:
Woda-Środowisko-Obszary Wiejskie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Effect of uniaxial compression on water retention, hydraulic conductivity and the penetration resistance of six Greek soils
Autorzy:
Panayiotopoulos, K.P.
Salonikiou, E.
Siaga, K.
Germanopoulou, V.
Skaperda, S.
Powiązania:
https://bibliotekanauki.pl/articles/26633.pdf
Data publikacji:
2003
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
hydraulic conductivity
uniaxial compression
Greece
penetration resistance
Greek soil
water retention
Źródło:
International Agrophysics; 2003, 17, 4
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Hydrophysical characteristics and evaporation of Haplic Luvisol and Mollic Gleysol aggregates
Autorzy:
Witkowska-Walczak, B.
Powiązania:
https://bibliotekanauki.pl/articles/24599.pdf
Data publikacji:
2003
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
soil aggregation
evaporation
water conductivity
water
aggregate size
soil aggregate
water capacity
Źródło:
International Agrophysics; 2003, 17, 3
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Simultaneous measurement of oxygen flux and salinity of the water saturated mineral soils
Autorzy:
Bieganowski, A.
Powiązania:
https://bibliotekanauki.pl/articles/24164.pdf
Data publikacji:
2003
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
mineral soil
simultaneous measurement
electrical conductivity
saturated soil
oxygen flux
soil oxygen
soil salinity
water
salinity
flux density
Źródło:
International Agrophysics; 2003, 17, 3
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Changes in the hydrophysical properties of peat soils under anthropogenic evolution
Autorzy:
Rovdan, E.
Witkowska-Walczak, B.
Walczak, R.
Slawinski, C.
Powiązania:
https://bibliotekanauki.pl/articles/24801.pdf
Data publikacji:
2002
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
hydraulic conductivity
peat soil
hydrophysical property
anthropogenic evolution
water retention
Źródło:
International Agrophysics; 2002, 16, 3
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Spatial characteristics of water conductivity in the surface level of Polish arable soils
Autorzy:
Walczak, R
Ostrowski, J.
Witkowska-Walczak, B.
Slawinski, C.
Powiązania:
https://bibliotekanauki.pl/articles/26447.pdf
Data publikacji:
2002
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
surface level
Polska
water permeability
soil
water conductivity
water retention
arable soil
water balance
Źródło:
International Agrophysics; 2002, 16, 3
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Przewodnosc hydrauliczna osrodka porowatego w ujeciu statystycznym
Autorzy:
Usowicz, B
Powiązania:
https://bibliotekanauki.pl/articles/1402599.pdf
Data publikacji:
2001
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
osrodki porowate
porowatosc gleby
woda glebowa
retencja wodna
przewodnosc hydrauliczna
porous medium
soil porosity
soil water
water retention
hydraulic conductivity
Źródło:
Acta Agrophysica; 2001, 53; 177-187
1234-4125
Pojawia się w:
Acta Agrophysica
Dostawca treści:
Biblioteka Nauki
Artykuł

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