Interrelationship between soil depth and soil properties of Pieniny National Park forest(Poland)
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摘要
The purpose of this research was to investigate the relationship between soil biota such as microbial activity, soil fauna(e.g., earthworms and enchytraeids), and soil physical and chemical properties. The study area was located in Pieniny National Park(PNP) in the Carpathian Mountains in southern Poland. Soil samples were collected from six forest monitoring areas of PNP from two soil layers(at 0–15 cm and 15–30 cm down, respectively). The investigated soils were classified to eutric cambisols and had silt or silt loam soil texture. Upon analysis, soil aggregate stability index was connected with other physical, chemical, and biological soil properties.It was noted that the stability index of 3 mm to 5 mm soil aggregates influenced pH and dissolved organic carbon. The stability index of 2 mm to 3 mm soil aggregates was positively correlated with dissolved organic carbon, soil moisture, microbial biomass carbon, total organic carbon, total nitrogen, and enchytraeid density, and negatively correlated with bulk density, particle density, porosity, and permanent wilting point. The stability index of 1 mm to 2 mm soil aggregates was positively correlated with total nitrogen, enchytraeid and earthworm density and negatively correlated with particle density, porosity, and permanent wilting point. The study has shown what factors create a stable soil structure in the forest soils of PNP.
The purpose of this research was to investigate the relationship between soil biota such as microbial activity, soil fauna(e.g., earthworms and enchytraeids), and soil physical and chemical properties. The study area was located in Pieniny National Park(PNP) in the Carpathian Mountains in southern Poland. Soil samples were collected from six forest monitoring areas of PNP from two soil layers(at 0–15 cm and 15–30 cm down, respectively). The investigated soils were classified to eutric cambisols and had silt or silt loam soil texture. Upon analysis, soil aggregate stability index was connected with other physical, chemical, and biological soil properties.It was noted that the stability index of 3 mm to 5 mm soil aggregates influenced pH and dissolved organic carbon. The stability index of 2 mm to 3 mm soil aggregates was positively correlated with dissolved organic carbon, soil moisture, microbial biomass carbon, total organic carbon, total nitrogen, and enchytraeid density, and negatively correlated with bulk density, particle density, porosity, and permanent wilting point. The stability index of 1 mm to 2 mm soil aggregates was positively correlated with total nitrogen, enchytraeid and earthworm density and negatively correlated with particle density, porosity, and permanent wilting point. The study has shown what factors create a stable soil structure in the forest soils of PNP.
The purpose of this research was to investigate the relationship between soil biota such as microbial activity, soil fauna(e.g., earthworms and enchytraeids), and soil physical and chemical properties. The study area was located in Pieniny National Park(PNP) in the Carpathian Mountains in southern Poland. Soil samples were collected from six forest monitoring areas of PNP from two soil layers(at 0–15 cm and 15–30 cm down, respectively). The investigated soils were classified to eutric cambisols and had silt or silt loam soil texture. Upon analysis, soil aggregate stability index was connected with other physical, chemical, and biological soil properties.It was noted that the stability index of 3 mm to 5 mm soil aggregates influenced pH and dissolved organic carbon. The stability index of 2 mm to 3 mm soil aggregates was positively correlated with dissolved organic carbon, soil moisture, microbial biomass carbon, total organic carbon, total nitrogen, and enchytraeid density, and negatively correlated with bulk density, particle density, porosity, and permanent wilting point. The stability index of 1 mm to 2 mm soil aggregates was positively correlated with total nitrogen, enchytraeid and earthworm density and negatively correlated with particle density, porosity, and permanent wilting point. The study has shown what factors create a stable soil structure in the forest soils of PNP.
引文
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Bronick CJ,Lal R(2005)Soil structure and management:Areview.Geoderma 124(1-2):3-22.https://doi.org/10.1016/j.geoderma.2004.03.005
Brown GG,Barois I,Lavelle P(2000)Regulation of soil organic matter dynamics and microbial activity in the drilosphere and the role of interactions with other edaphic functional domainss.European Journal of Soil Biology 36(3-4):177-198.https://doi.org/10.1016/S1164-5563(00)01062-1
Bryk M,Ko?odziej B,S?owińska-Jurkiewicz A,et al.(2017)Evaluation of soil structure and physical properties influenced by weather conditions during autumn-winter-spring season.Soil and Tillage Research 170:66-76.https://doi.org/10.1016/j.still.2017.03.004
Bullinger-Weber G,Le Bayon RC,Guenat C,et al.(2007).Influence of some physicochemical and biological parameters on soil structure formation in alluvial soils.European Journal of Soil Biology 43(1):57-70.https://doi.org/10.1016/j.ejsobi.2006.05.003
Burri K,Graf F,B?ll A(2009)Revegetation measures improve soil aggregate stability?:a case study of a landslide area in Central Switzerland.Forest Snow and Landscape Research82(1):45-60.
Casida LE,Klein DA,Santoro T(1964)Soil dehydrogenase activity.Soil Science 98(6):371-376.
Chan KY,Bowman A,Oates A(2001)Oxidizible organic carbon fractions and soil quality changes in an oxic paleustalf under different pasture leys.Soil Science 166(1):61-67.https://doi.org/10.1097/00010694-200101000-00009
Chenu C(1993)Clay-or sand-polysaccharide associations as models for the interface between micro-organisms and soil:water related properties and microstructure.Geoderma 56(1-4):143-156.https://doi.org/10.1016/0016-7061(93)90106-U
Dimoyiannis DG,Tsadilas CD,Valmis S(1998)Factors affecting aggregate instability of Greek agricultural soils.Communications in Soil Science and Plant Analysis 29(9-10):1239-1251.https://doi.org/10.1080/00103629809370023
Don A,Steinberg B,Sch?ning I,et al.(2008)Organic carbon sequestration in earthworm burrows.Soil Biology and Biochemistry 40(7):1803-1812.https://doi.org/10.1016/j.soilbio.2008.03.003
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