scholarly journals Long-Term Effects of Tillage on Soil Chemical Properties and Grain Yields of a Dryland Winter Wheat-Sorghum/Corn-Fallow Rotation in the Great Plains

2006 ◽  
Vol 98 (1) ◽  
pp. 26-33 ◽  
Author(s):  
David D. Tarkalson ◽  
Gary W. Hergert ◽  
Kenneth G. Cassman
Keyword(s):  
Winter Wheat ◽  
Great Plains ◽  
Chemical Properties ◽  
Soil Chemical Properties ◽  
Long Term Effects ◽  
Grain Yields

scholarly journals Agricultural abandonment in Mediterranean reclaimed peaty soils: long-term effects on soil chemical properties, arbuscular mycorrhizas and CO2 flux

2015 ◽  
Vol 199 ◽  
pp. 164-175 ◽  
Author(s):  
Elisa Pellegrino ◽  
Simona Bosco ◽  
Valentina Ciccolini ◽  
Chiara Pistocchi ◽  
Tiziana Sabbatini ◽  
...  
Keyword(s):  
Chemical Properties ◽  
Co2 Flux ◽  
Arbuscular Mycorrhizas ◽  
Soil Chemical Properties ◽  
Long Term Effects ◽  
Agricultural Abandonment

Effects of long-term bare fallow during the winter-wheat growth season on the soil chemical properties, fungal community composition and the occurrence of maize fungal diseases in North China

Plant Disease ◽  
2021 ◽  
Author(s):  
Yajiao Wang ◽  
Lijing Ji ◽  
Qiusheng Li ◽  
yu xing wu ◽  
Congcong Li ◽  
...  
Keyword(s):  
Winter Wheat ◽  
Fungal Community ◽  
Chemical Properties ◽  
Soil Chemical Properties ◽  
Fungal Community Composition ◽  
Nitrogen And Phosphorus ◽  
Growth Season ◽  
Available Nitrogen ◽  
Bare Fallow

On the North China Plain, one of the most water-deficient regions in China, bare fallow has been implemented over a large-scale area to conserve water during the growth season of water-intensive winter wheat since 2015. However, the effects of this bare fallow on fungal community and the occurrence of crop diseases are poorly understood. Here we measured soil chemical properties, fungal community composition and the occurrence of crop diseases after 15 years of long-term fallow (continuous maize or soybean) and non-fallow (maize-wheat rotation; soybean-wheat rotation) cropping systems. Bare fallow during the winter-wheat growth season significantly decreased soil organic matter, available nitrogen and phosphorus. It also changed the composition of soil fungal communities, i.e., increased relative abundances of some potentially pathogenic species of Lectera, Fusarium and Volutella but decreased beneficial Cladorrhium and Schizothecium. Meanwhile, the epidemic tendency of maize diseases changed correspondingly: the disease index of southern corn leaf blight and maize brown spot increased, but the incidence of stalk rot decreased compared with the non-fallow system. Soybean diseases were very mild regardless of the cropping system during the total experimental period. Network analysis demonstrated that the soil fungal diversity associated with maize diseases was affected by the decreased soil organic matter and available nitrogen and phosphorus. Our results suggest that bare fallow in winter-wheat season affected the soil chemical properties, fungal community and the occurrence of maize fungal diseases.

Cropping system influences on soil chemical properties and soil quality in the Great Plains

2006 ◽  
Vol 21 (1) ◽  
pp. 26-35 ◽  
Author(s):  
M.M. Mikha ◽  
M.F. Vigil ◽  
M.A. Liebig ◽  
R.A. Bowman ◽  
B. McConkey ◽  
...  
Keyword(s):  
Great Plains ◽  
Cropping Systems ◽  
Chemical Properties ◽  
Cropping System ◽  
Soil Chemical Properties ◽  
Total N ◽  
Organic C ◽  
General Chemical ◽  
Study Sites

AbstractSoil management and cropping systems have long-term effects on agronomic and environmental functions. This study examined the influence of contrasting management practices on selected soil chemical properties in eight long-term cropping system studies throughout the Great Plains and the western Corn Belt. For each study, soil organic C (SOC), total N (TN), particulate organic matter (POM), inorganic N, electrical conductivity (EC), and soil pH were evaluated at 0–7.5, 7.5–15, and 15–30 cm within conventional (CON) and alternative (ALT) cropping systems for 4 years (1999–2002). Treatment effects were primarily limited to the surface 7.5 cm of soil. No-tillage (NT) and/or elimination of fallow in ALT cropping systems resulted in significantly (P<0.05) greater SOC and TN at 0–7.5 cm within five of the eight study sites [Akron, Colorado (CO); Bushland, Texas (TX); Fargo, North Dakota (ND); Mandan, ND; and Swift Current, Saskatchewan (SK), Canada]. The same pattern was observed with POM, where POM was significantly (P<0.05) greater at four of the eight study sites [Bushland, TX, Mandan, ND, Sidney, Montana (MT), and Swift Current, SK]. No consistent pattern was observed with soil EC and pH due to management, although soil EC explained almost 60% of the variability in soil NO3-N at 0–7.5 cm across all locations and sampling times. In general, chemical soil properties measured in this study consistently exhibited values more conducive to crop production and environmental quality in ALT cropping systems relative to CON cropping systems.

Effects of Long‐Term, Annual Applications of N and P on Corn Grain Yields and Soil Chemical Properties 1

1983 ◽  
Vol 75 (1) ◽  
pp. 94-99 ◽  
Author(s):  
M. L. Hooker ◽  
R. E. Gwin ◽  
G. M. Herron ◽  
P. Gallagher
Keyword(s):  
Chemical Properties ◽  
Soil Chemical Properties ◽  
Grain Yields ◽  
Corn Grain

LONG-TERM EFFECT OF DEEP PLOWING SOLONETZIC SOIL ON CHEMICAL CHARACTERISTICS AND CROP YIELD

1990 ◽  
Vol 70 (4) ◽  
pp. 565-570 ◽  
Author(s):  
D. W. McANDREW ◽  
S. S. MALHI
Keyword(s):  
Crop Yield ◽  
Crop Yields ◽  
Chemical Properties ◽  
Soil Chemical Properties ◽  
Long Term Effects ◽  
Long Term Effect ◽  
Solonetzic Soil ◽  
Ap Horizon ◽  
Deep Plowing

Deep plowing (DP) has been investigated as a possible ameliorative procedure for Solonetzic soils, but the long-term effects of DP on soil properties are not known. Soil sampling to determine the long-lasting effects of DP on some soil chemical properties and crop yields was conducted at four sites with Solonetzic soils in east-central Alberta. The soils had been deep plowed 11–29 yr prior to sampling. Compared to adjacent unplowed (check) treatments, DP resulted in significant improvements in soil chemical properties at most of the sites. The sodium adsorption ratio (SAR) of the AB horizon (12- or 15- to 30-cm depth) was lower after DP at all four sites. Extractable and soluble Ca increased in the Ap horizon (0–12 cm) of DP soils, whereas extractable Na decreased in the Ap or AB horizons at three sites. The pH of the Ap horizon increased from acidic to neutral at three sites, while EC of the Ap horizon decreased at two sites. Crop yield increased due to DP at the three sites where yields were measured. The results indicate a long-term amelioration of Solonetzic soils by DP. Key words: Amelioration, deep plowing, deep tillage, sodic soil

scholarly journals Long-Term Effects of Amendment with Olive Mill Wastewater on Soil Chemical Properties, Microbial Community, and Olive Tree Vegetative and Productive Activities

Agronomy ◽  
2021 ◽  
Vol 11 (12) ◽  
pp. 2562
Author(s):  
Luca Regni ◽  
Daniela Pezzolla ◽  
Simona Ciancaleoni ◽  
Giorgio Marozzi ◽  
Emidio Albertini ◽  
...  
Keyword(s):  
Microbial Community ◽  
Chemical Properties ◽  
Olive Tree ◽  
Olive Mill Wastewater ◽  
Soil Chemical Properties ◽  
Available Phosphorus ◽  
Long Term Effects ◽  
Organic C ◽  
Olive Mill

The long-term effects of the olive mill wastewater (OMWW) spreading on soil chemical properties, microbial community, and olive tree parameters have been far poorly investigated. Therefore, this study aims to evaluate the effect of OMWW application on an olive orchard, and samples were collected at two different depths (0–20 cm and 20–40 cm) and 14 days, one year and two years from the end of the OMWW spreading on soil chemical characteristics and soil microbial structures. Variations of soil chemical parameters (pH, salinity, available P, and water-extractable organic C) were observed particularly at 14 days after spreading at both depths. All these parameters reached similar values to the soil after two years, except for available phosphorus. Firmicutes, Proteobacteria, and Actinobacteria are the most abundant phyla: only Firmicutes were negatively affected by the OMWW spreading after 14 days, suggesting that Gram-positive bacteria were probably negatively influenced by the addition of OMWW. The abundance of bacterial taxa in the soil is restored along time, except for the decrease of Firmicutes. This evidence suggests that the OMWW spreading in the long term does not affect the endemic soil bacterial community of the olive grove, as well as leaf net photosynthesis, the olive tree vegetative activity, yield, and fruits characteristics.

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