Mineral fertilization and soil depth slightly affected aggregate structures despite significantly altered microbial properties in surface forest soils

2020 ◽  
Vol 20 (10) ◽  
pp. 3615-3626
Author(s):  
Yun Niu ◽  
Manyun Zhang ◽  
Shahla Hosseini Bai ◽  
Zhihong Xu ◽  
Yuanqiu Liu ◽  
...  
Keyword(s):  
Forest Soils ◽  
Soil Depth ◽  
Mineral Fertilization ◽  
Microbial Properties ◽  
Aggregate Structures

scholarly journals Profiles of C- and N-trace gas production in N-saturated forest soils

2005 ◽  
Vol 2 (4) ◽  
pp. 1127-1157 ◽  
Author(s):  
K. Butterbach-Bahl ◽  
U. Berger ◽  
N. Brüggemann ◽  
J. Duyzer
Keyword(s):  
Forest Soils ◽  
Forest Floor ◽  
Soil Depth ◽  
Douglas Fir ◽  
Anaerobic Incubation ◽  
N2o Production ◽  
Time Activity ◽  
Soil Layers ◽  
Clear Cut ◽  
First Time

Abstract. This study provides for the first time data on the stratification of NO and N2O production with soil depth under aerobic and anaerobic incubation conditions for different temperate forest sites in Germany (spruce, beech, clear-cut) and the Netherlands (Douglas fir). Results show that the NO and N2O production activity is highest in the forest floor and decreases exponentially with increasing soil depth. Under anaerobic incubation conditions NO and N2O production was in all soil layers up to 2-3 orders of magnitude higher then under aerobic incubation conditions. Furthermore, significant differences between sites could be demonstrated with respect to the magnitude or predominance of NO and N2O production. These were driven by stand properties (beech or spruce) or management (clear-cut versus control). With regard to CH4 the most striking result was the lack of CH4 uptake activity in soil samples taken from the Dutch Douglas fir site at Speulderbos, which is most likely a consequence of chronically high rates of atmospheric N deposition. In addition, we could also demonstrate that CH4 fluxes at the soil surface are obviously the result of simultaneously occurring uptake and production processes, since even under aerobic conditions a net production of CH4 in forest floor samples was found. The provided dataset will be very useful for the development and testing of process oriented models, since for the first time activity data stratified for several soil layers for N2O, NO, and CH4 production/oxidation activity for forest soils are provided.

scholarly journals Drought and rewetting events enhance nitrate leaching and seepage-mediated translocation of microbes from beech forest soils

2020 ◽  
Author(s):  
Markus Krüger ◽  
Karin Potthast ◽  
Beate Michalzik ◽  
Alexander Tischer ◽  
Kirsten Küsel ◽  
...  
Keyword(s):  
Forest Soils ◽  
Nitrate Leaching ◽  
Soil Depth ◽  
Groundwater Resources ◽  
Beech Forest ◽  
Summer Drought ◽  
Ammonia Oxidizing Bacteria ◽  
Litter Layer ◽  
Drought Period ◽  
Potential Nitrification

AbstractNitrification in forest soils is often associated with increased leaching of nitrate to deeper soil layers with potential impacts on groundwater resources, further enhanced under scenarios of anthropogenic atmospheric nitrogen deposition and predicted weather extremes. We aimed to disentangle the relationships between soil nitrification potential, seepage-mediated nitrate leaching and the vertical translocation of nitrifiers in soils of a temperate mixed beech forest in central Germany before, during and after the severe summer drought 2018. Leaching of nitrate assessed below the litter layer and in 4, 16 and 30 cm soil depth showed high temporal and vertical variation with maxima at 16 and 30 cm during and after the drought period. Maximum of soil potential nitrification activity of 4.4 mg N kg-1 d-1 only partially coincided with maximum nitrate leaching of 10.5 kg N ha-2. Both ammonia oxidizing bacteria (AOB) and ammonia oxidizing archaea (AOA) were subject to translocation by seepage, and AOB decreased at least by half and AOA increased by one to three orders of magnitude in their abundance in seepage with increasing soil depth. On the level of the total bacterial population, an increasing trend with depth was also observed for Cand. Patescibacteria while Bacteroidetes were strongly mobilized from the litter layer but poorly transported further down. Despite stable population densities in soil over time, abundances of AOA, AOB and total bacteria in seepage increased by one order of magnitude after the onset of autumn rewetting. Predicted future higher frequency of drought periods in temperate regions may result in more frequent seepage-mediated seasonal flushes of nitrate and bacteria from forest soils. Moreover, the observed translocation patterns point to taxon-specific differences in the susceptibility to mobilization, suggesting that only selected topsoil derived microbial groups are likely to affect subsoil or groundwater microbial communities and their functional potential.

scholarly journals Soil Carbon Sequestrations in Forest Soils in Relation to Parent Material and Soil Depth in South-Eastern Nigeria

2020 ◽  
Vol 09 (04) ◽  
pp. 400-409
Author(s):  
Chinonso Millicent Chris-Emenyonu ◽  
Emmanuel Uzoma Onweremadu ◽  
John Didacus Njoku ◽  
Chioma Mildred Ahukaemere ◽  
Benarden Ngozi Aririguzo
Keyword(s):  
Soil Carbon ◽  
Forest Soils ◽  
Soil Depth ◽  
Parent Material ◽  
South Eastern

scholarly journals Heavy metals in pastureland soils situated in A Pastoriza (NW Spain) treated with cattle slurry and NPK fertilizers

2015 ◽  
Vol 5 ◽  
Author(s):  
Natalia Seco-Reigosa ◽  
María J. Fernández-Sanjurjo ◽  
Avelino Núñez-Delgado ◽  
Laura Cutillas-Barreiro ◽  
Antía Gómez-Armesto ◽  
...  
Keyword(s):  
Heavy Metals ◽  
Heavy Metal ◽  
Forest Soils ◽  
Soil Depth ◽  
Available P ◽  
Cattle Slurry ◽  
Nw Spain ◽  
Npk Fertilizers ◽  
Pasture Production ◽  
Total Concentrations

In Galicia (NW Spain), pasturelands cover a broad extension and are mainly used to feed cattle. Farms are managed in an intensive manner, using cattle slurry and inorganic fertilizers to increase pasture production, but also increasing risks of heavy metal pollution. In this work we studied the influence of fertilization practices on total concentrations and in-depth distribution of heavy metals and related elements (As, Cd, Cr, Cu, Mn, Ni, Pb and Zn) in two forest soils (SN1, SN2) and five pastureland soils (P1-P5) fertilized with cattle slurry and NPK, in a broadly exploded farmland area (A Pastoriza, Lugo). Soils SN2 and P4 were developed over slate, whereas soils SN1, P1, P2, P3 and P5 evolved on Candana quartzite. Forest soils presented acid pH (4.58-4.68), high Al saturation (75-90%), and low available P concentration (4.78-11.96 mg kg<sup>-1</sup>), whereas those parameters exhibited better scores in the pastureland soils, due to previous amendment and fertilization practices, thus giving pH 5.17-7.02, Al saturation 0.58-59.24%, and available P 5.24-42.07 mg kg<sup>-1</sup>. Regarding heavy metals, soil depth did not affect significantly to total concentrations, contrary to that happening with parent material, with higher As, Cu, Fe, and Ni concentrations found in soils over slate (possibly due to the presence of pyritic materials). In most cases, heavy metal total concentrations were lower than that considered as reference background levels for soils developed over each of the parent materials, and were always lower than that considered phyto-toxic. In this study, natural soils usually presented heavy metal total contents similar or even higher than that of the fertilized soils (unless Zn in the P4 pastureland), thus indicating that the spread doses of fertilizers did not influence significantly their concentration levels.

scholarly journals Effect of Digestate on Soil Organic Carbon and Plant-Available Nutrient Content Compared to Cattle Slurry and Mineral Fertilization

Agronomy ◽  
2020 ◽  
Vol 10 (3) ◽  
pp. 379 ◽  
Author(s):  
Przemysław Barłóg ◽  
Lukáš Hlisnikovský ◽  
Eva Kunzová
Keyword(s):  
Organic Carbon ◽  
Soil Organic Carbon ◽  
Soil Depth ◽  
Nutrient Content ◽  
Fertilizer Treatment ◽  
Cattle Slurry ◽  
Mineral Fertilization ◽  
Mineral N ◽  
Effect Of Treatment ◽  
K Fertilization

Digestate contains many valuable nutrients, including nitrogen (N), phosphorus (P), and potassium (K); however, it is characterized by relatively little organic matter. The objective of this study was to assess the four-year impact of digestate (Dig) application, digestate + straw (Dig + St), cattle slurry (Csl), and mineral fertilization (NPK) on soil organic carbon (SOC), total nitrogen (TN), mineral N (Nmin), and the content of plant-available P and K. Fertilization did not have any significant influence on SOC, TN, and SOC/TN parameters. Yet, in comparison with control, there was an upward trend in the concentration of SOC and TN in the topsoil, where fertilizers were applied. In contrast to SOC and TN, fertilizer treatment significantly affected the content of P, K, and Nmin, and the differences depended on the soil depth and the fertilizer used. On average, the highest content of P was obtained in Csl treatment, but the highest content of K was observed in Dig + St. The effect of treatment on Nmin in spring was as follows: NPK = control < Csl = Dig + St < Dig. Straw plowing increased the bio-immobilization of N with digestate and, at the same time, lowered the content level of nitrates in soil.

scholarly journals Nitrogen fluxes from irrigated common‑bean as affected by mulching and mineral fertilization

2013 ◽  
Vol 48 (5) ◽  
pp. 478-486 ◽  
Author(s):  
Márcia Thaís de Melo Carvalho ◽  
Beáta Emöke Madari ◽  
Wesley Gabriel de Oliveira Leal ◽  
Adriana Rodolfo da Costa ◽  
Pedro Luiz Oliveira de Almeida Machado ◽  
...  
Keyword(s):  
Common Bean ◽  
Soil Depth ◽  
Growing Season ◽  
N Fertilization ◽  
Mineral Fertilization ◽  
Intergovernmental Panel ◽  
N Losses ◽  
Nitrogen Fluxes ◽  
Signal Grass ◽  
Crop System

The objective of this work was to measure the fluxes of N2O‑N and NH3‑N throughout the growing season of irrigated common‑bean (Phaseolus vulgaris), as affected by mulching and mineral fertilization. Fluxes of N2O‑N and NH3‑N were evaluated in areas with or without Congo signal grass mulching (Urochloa ruziziensis) or mineral fertilization. Fluxes of N were also measured in a native Cerrado area, which served as reference. Total N2O‑N and NH3‑N emissions were positively related to the increasing concentrations of moisture, ammonium, and nitrate in the crop system, within 0.5 m soil depth. Carbon content in the substrate and microbial biomass within 0.1 m soil depth were favoured by Congo signal grass and related to higher emissions of N2O‑N, regardless of N fertilization. Emission factors (N losses from the applied mineral nitrogen) for N2O‑N (0.01-0.02%) and NH3‑N (0.3-0.6%) were lower than the default value recognized by the Intergovernmental Panel on Climate Change. Mulch of Congo signal grass benefits N2O‑N emission regardless of N fertilization.

Changes in soil physicochemical and microbial properties along elevation gradients in two forest soils

2016 ◽  
Vol 31 (3) ◽  
pp. 242-253 ◽  
Author(s):  
Lei Hu ◽  
Zeyu Xiang ◽  
Genxu Wang ◽  
Rashad Rafique ◽  
Wei Liu ◽  
...  
Keyword(s):  
Forest Soils ◽  
Elevation Gradients ◽  
Microbial Properties

scholarly journals Characterization of Phosphorus in a Toposequence of Subtropical Perhumid Forest Soils Facing a Subalpine Lake

2018 ◽  
Author(s):  
Yo-Jin Shiau ◽  
Chung-Wen Pai ◽  
Jeng-Wei Tsai ◽  
Wen-Cheng Liu ◽  
Rita S.W. Yam ◽  
...  
Keyword(s):  
Forest Soils ◽  
31P Nmr ◽  
Soil Depth ◽  
Critical Factor ◽  
Chemical Extraction ◽  
Chemical Fractionation ◽  
Oxide Content ◽  
Inorganic P ◽  
Fe Oxide ◽  
Soil P

The productivity of forests is often considered to be limited by the availability of phosphorus (P). Knowledge of the role of organic and inorganic P in humid subtropical forest soils is lacking. In this study, we used chemical fractionation and 31P nuclear magnetic resonance (NMR) spectroscopy to characterize the form of P and its distribution in undisturbed perhumid Chamaecyparis forest soils. The toposequence of transects was investigated for the humic layer from summit to footslope and lakeshore. The clay layer combined with a placic-like horizon in the subsoil may affect the distribution of soil P because both total P and organic P (Po) contents in all studied soils decreased with soil depth. In addition, Po content was negatively correlated with soil crystalline Fe oxide content, whereas inorganic P (Pi) content was positively correlated with soil crystalline Fe oxide content and slightly increased with soil depth. Thus, Pi may be mostly adsorbed by soil crystalline Fe oxides in the soils. Among all extractable P fractions, the NaOH-Po fraction appeared to be the major component, followed by NaHCO3-Po; the resin-P and HCl-Pi fractions were lowest. In addition, we found no typical trend for Pi and Po contents in soils with topographical change among the three sites. From the 31P-NMR spectra, the dominant Po form in soils from all study sites was monoesters with similar spectra. The 31P-NMR findings were basically consistent with those from chemical extraction. Soil formation processes may be the critical factor affecting the distribution of soil P. High precipitation and year-round high humidity may be important in the differentiation of the P species in this landscape.

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