Comparative effectiveness of phosphate-enriched compost and single superphosphate on yield, uptake of nutrients and soil quality under soybean–wheat rotation

2001 ◽  
Vol 137 (1) ◽  
pp. 45-54 ◽  
Author(s):  
M. C. MANNA ◽  
P. K. GHOSH ◽  
B. N. GHOSH ◽  
K. N. SINGH

Low organic matter concentration coupled with low native soil phosphorus (P) concentrations is a major constraint limiting the productivity of a soybean–wheat system on Vertisols in the Indian semi-arid tropics. In a 3-year field study (1996–99), the performance of four different composts obtained from legume straw (Glycine max Merr.L), cereal straw (Triticum aestivum), oilseed straw (Brassica juncea L.) and city rubbish were compared, and also with chemical fertilizers in terms of degree of maturity, quality of compost, improvement in soil organic matter, biological activities of soil and yields of soybean and wheat. Phospho-sulpho-nitrocomposts (phosphocomposts) were prepared containing approximately 2·5 to 4·2% P and 1·4 to 2·3% N, in an aerobic decomposition process for 4 months by adding an aqueous slurry of 1:1 (dry weight) cow dung, 2·2% P in the form of low grade Mussorie phosphate rock (7·5% P), 10% pyrite (S, 22·2%) and 0·5% urea N, and bioinoculums such as the cellulose decomposers Paecilomyces fusisporus and Aspergillus awamori, and P-solubilizing organisms i.e. Bacillus polymyxa and Pseudomonas striata. The maturity indexes were strongly associated with the source of materials, chemical composition and degree of decomposition. The matured composts had lower C/N ratios (8·2 to 21·7) and water soluble carbohydrates (0·23 to 0·43%) and larger ratios of cation exchange capacity/total organic carbon (CEC/TOC) and lignin/cellulose than the initial. The matured compost increased total P, water soluble P, citrate soluble P, total N and NO3-N and the application of phosphocompost at the rate of 10 t/ha gave plant growth dry matter accumulation, seed yield and P uptake by soybean equivalent to single superphosphate at 26·2 kg P/ha. The continuous turnover of enriched phosphocompost increased soil microbial biomass C and the activity of enzymes compared to application of chemical fertilizer.

2017 ◽  
Vol 7 ◽  
Author(s):  
Laura Antonela Iturri ◽  
Graciela Gloria Hevia ◽  
Montserrat Diaz Raviña ◽  
Daniel Eduardo Buschiazzo

Stable and labile soil organic compounds play different roles in the soil. It is a question of how far soil organic matter (SOM) fractions with different labilities vary as a function of climatic and management conditions. In order to answer this question stable (organic C -C-, total N -N-, organic P -Po-), and labile SOM fractions (total carbohydrates -CHt- and hot water soluble carbohydrates -CHw-) were measured monthly for two years in the 10-cm soil top-layer of an Entic Haplustoll, under conventional tillage (CT), vertical tillage (VT) and no-till (NT). Results showed that contents of all analyzed organic fractions were higher in NT than in VT and CT in almost all sampling dates. All organic compounds were less variable with time in NT and VT than in CT, in agreement with the smaller soil disturbance of NT and VT compared to CT. The more labile fractions varied as a function of short term changes in the climatic conditions, mainly temperature. Under soil disturbing tillage systems, the most stable fractions tended to decrease and the more labile to increase with time. This was attributed to the transformation of the more stable into the more labile fractions, possibly due to the disruption of aggregates produced by tillage that favored SOM mineralization. Po was the less variable compound, even under the most disturbing tillage conditions. The quotients C/N, CHt/C and CHw/C evolved similarly in all tillage systems, indicating that that tillage systems change the amount but not the quality of SOM.


2001 ◽  
Vol 58 (1) ◽  
pp. 165-170 ◽  
Author(s):  
Luís Ignácio Prochnow ◽  
José Francisco da Cunha ◽  
Ariel Francisco Candiotti Ventimiglia

Ten P fertilizers were collected (commercial fertilizers) or synthesized (experimental sources) in order to obtain single superphosphates varying in water and citrate solubility. A standard source of P was also produced by crystallization of the water-soluble fraction of a triple superphosphate. Eleven P sources were band applied to a medium textured Xanthic Hapludox, in Bahia, Brazil (low content of resin-extractable P) at a rate of 80 kg ha-1 of NAC + H2O (neutral ammonium citrate plus water) soluble P2O5, with soybean as the crop which was grown to maturity. A check plot (control) was included in the study. Three of the P sources [single superphosphate produced from Araxa phosphate rock (PR), low-grade single superphosphate produced from Lagamar PR and the standard source of P] were also applied at rates to provide 40 and 120 kg ha-1 of NAC + H2O soluble P2O5. Yield of soybean was evaluated by analysis of variance with mean comparison performed utilizing LSD lines, considering the P sources applied at a rate of 80 kg ha-1 of P2O5 + control. Regression procedures were used to study the relation between yield of soybean and rates of P2O5. The fertilizers tested performed equally well as a source of P for soybean. The level of water-soluble P did not influence fertilizer performance.


1983 ◽  
Vol 55 (4) ◽  
pp. 345-354
Author(s):  
Helinä Hartikainen

The effect of increasing lime quantities on reactions of native and applied P was investigated in an incubation experiment performed with two acid mineral soils of pH 4.8 (CaCl2). The soil samples differed considerably in the content of organic matter, which was reflected in their pH buffering power: in the fine sand, rich in organic matter (6.4 % org. C), liming raised the pH less than in the muddy fine sand (3.0 % org. C). The level of native water-soluble P was markedly lowered in the incubated soil samples treated with nutrient salts. In the muddy fine sand, the decrease tended to be the smaller, whereas in the fine sand the greater, the more intensive liming was. This held true also of added P. The changes in CHANG and JACKSON’s P fractions did not alone satisfactorily explain the dissimilar response of soil P to lime treatments. The fate of P was concluded to be controlled by the quality and quantity of Al species differing in their affinity for P sorption. The changes in the solubility of P are a net result of processes enhancing and of those depressing the sorption tendency. In the fine sand soil of high initial content of water-soluble P, the detrimental effect of liming seemed to be attributed to the abundance of polymerized Al the affinity of which for P retention increased with intensified liming. Further, the high pH buffering power of this soil reduced the efficiency of lime to produce OH- ions able to compete with phosphate for sorption sites. In the muddy fine sand soil, on the contrary, the formation of sorption-active sites was not equally marked and, owing to the weaker pH buffering, liming raised the OH- concentration more effectively.


2003 ◽  
Vol 19 (3-4) ◽  
pp. 61-69
Author(s):  
Jan Pyś ◽  
Wladislaw Migdal ◽  
Branislav Zivkovic ◽  
Olga Kosovac ◽  
Mihal Fabjan ◽  
...  

In the experiment, forage from the 1st cut of meadow grasses mown at the heading stage of dominant grasses was ensiled. The control silages were made from fresh forage (dry matter 223.5 g?kg-1) and wilted forage (dry matter 351.9 g?kg-1). The experimental silages were made from fresh forages supplemented with a 5% water solution of lactic acid (0.5 and 0.7 l?100 kg-1 of forage) and 8% water solution of lactic acid (0.4 and 0.6 l?100 kg-1 of forage). The highest contents of crude protein, water-soluble carbohydrates and energy were found in silages supplemented with 5% lactic acid applied at 0.7 l?100 kg-1 of forage and in silages supplemented with 8% lactic acid applied at 0.6 l?100 kg-1 of forage. The above silage variants were also characterized by the lowest content of NH3-N in total-N, butyric acid and acetic acid, as well as the highest contents of lactic acid and the best indicators of fermentation quality. No important differences were found between silages made from wilted forage and silages made with lactic acid supplement.


1995 ◽  
Vol 10 (2) ◽  
pp. 82-87 ◽  
Author(s):  
C.P. Singh ◽  
A. Amberger

AbstractWe evaluated the effect of compost enriched with rock phosphate on the yield and phosphate nutrition of rye grass in a calcareous clay loam soil. Enriched compost was prepared by composting either Mussoorie rock phosphate (MP) or Hyper rock phosphate (HP) separately with wheat straw for up to 120 days. A significant amount of insoluble P was solubilized from both kinds of rock phosphates and converted to water soluble, organic, and formic acid soluble P fractions during composting. MP-enriched compost (MPEC) and HP-enriched compost (HPEC) contain 0.30% and 0.34% water soluble P205, 1.94% and 1.42% organic P2O5 2.82% and 3.28% formic acid soluble P2O5, and 1.76% and 1.18% insoluble P2O5, respectively. In a greenhouse study, the yield of ryegrass (three cuttings) with both enriched composts was not significantly different from that of single superphosphate fertilizer (SSP). Phosphorus fractions of soil before sowing and after harvesting the rye grass showed that fixation of P with native soil calcium was much higher with SSP than with enriched composts. No significant differences were observed between MRP and HRP.


1980 ◽  
Vol 60 (3) ◽  
pp. 517-525 ◽  
Author(s):  
P. A. ARP ◽  
H. B. KING ◽  
H. H. KRAUSE

Forest floor samples were obtained from three mature, even-aged, naturally regenerated conifer stands which varied with respect to drainage and indigenous soil fertility. Field moist subsamples were stored for 200 days in a refrigerator maintained at 4 °C and in a freezer maintained at − 10 °C; in addition, forest floor samples, dried at 60 °C for 48 h, were stored at room temperature. Subsamples were extracted initially and at predetermined time intervals with 2 N KCl (to determine mineral NH4+-N and NO3−-N), with neutral 1 N ammonium acetate (to determine water-soluble + exchangeable K, Ca, and Mg), and with distilled water (to determine soluble P). At 4 °C, extractable NH4+-N changed little during the first week of storage but increased steadily thereafter at rates which appeared to increase with increasing total N. Nitrification, present only in the sample taken from the most fertile site, commenced after 40 days of refrigerated storage. Concentrations of soluble P decreased initially, but rose thereafter at low, moderate, and high rates depending on total P. Freezing changed mineral NH4+-N to a minor extent, whereas NO3−-N was not affected. Concentrations of soluble P increased steadily during the first 2 mo of storage at − 10 °C. Levels of extractable K, Ca, and Mg were not affected by refrigeration and by length of storage time, but freezing increased extractable K considerably. Drying at 60 °C for 48 h produced abrupt increases in exchangeable + water-soluble nutrient levels. Further changes, however, were not observed during subsequent storage at room temperature.


2006 ◽  
Vol 96 (5) ◽  
pp. 861-869 ◽  
Author(s):  
David R. Yáñez-Ruiz ◽  
Nigel D. Scollan ◽  
Roger J. Merry ◽  
Charles J. Newbold

The present experiment was designed to estimate the quantitative contribution of rumen protozoa to the total N, conjugated linoleic acid (CLA) and vaccenic acid (VA;trans-11–18:1) flow to the duodenum of steers fed two silage diets: control silage (CS) and silage high in water-soluble carbohydrates (HS). Protozoal duodenal flows were estimated using a real-time PCR assay to quantify the genes encoding protozoal 18S ribosomal RNA. Denaturing gradient gel electrophoresis was used to confirm that the rumen protozoa populations were similar to the protozoal population flowing to the duodenum. Estimated duodenal flow of protozoal N was 14·2 and 18·2 g/d (P>0·05) for animals fed the CS and HS diets respectively. Protozoal flow thus represented between 12 and 15 % of the total N duodenal flow. In terms of fatty acid flow, protozoa accounted for between 30 and 43 % of the CLA and 40 % of the VA reaching the duodenum. The contribution of protozoa to 16:0 and 18:0 flows to the duodenum was less than 20 and 10 %, respectively. These results show that the fatty acids within protozoa make up a significant proportion of the CLA and VA reaching the duodenum of ruminants.


2015 ◽  
Vol 5 ◽  
Author(s):  
Alba Lombao ◽  
Montserrat Díaz Raviña ◽  
Ángela Martín ◽  
Ana Barreiro ◽  
María Teresa Fontúrbel ◽  
...  

Mulching treatment is often recommended <ins cite="mailto:Michele%20Francis" datetime="2015-01-23T16:22">in order </ins>to reduce post-fire erosion and sediment<del cite="mailto:Michele%20Francis" datetime="2015-01-23T15:45"></del> yields<ins cite="mailto:Michele%20Francis" datetime="2015-01-23T15:45">,</ins> but information concerning their effects on soil properties and hence on soil quality is scarce. In the present investigation<ins cite="mailto:Michele%20Francis" datetime="2015-01-23T16:22">,</ins> the influence of straw application on soil quality was evaluated <ins cite="mailto:Michele%20Francis" datetime="2015-01-23T16:22">on</ins><del cite="mailto:Michele%20Francis" datetime="2015-01-23T16:22"></del><del cite="mailto:Michele%20Francis" datetime="2015-01-23T15:46"> </del>hillslope shrubland <del cite="mailto:Michele%20Francis" datetime="2015-01-23T15:46"></del>in Saviñao (Lugo, NW Spain)<ins cite="mailto:Michele%20Francis" datetime="2015-01-23T15:47"> </ins><del cite="mailto:Michele%20Francis" datetime="2015-01-23T15:47"></del><del cite="mailto:Michele%20Francis" datetime="2015-01-23T15:46"></del><ins cite="mailto:Michele%20Francis" datetime="2015-01-23T15:46">th</ins><ins cite="mailto:Michele%20Francis" datetime="2015-01-23T16:02">a</ins><ins cite="mailto:Michele%20Francis" datetime="2015-01-23T15:46">t is </ins>susceptible to <del cite="mailto:Michele%20Francis" datetime="2015-01-23T15:46"></del>post-fire erosion (38% slope). In this area, <ins cite="mailto:Michele%20Francis" datetime="2015-01-23T16:04">which was </ins>affected by a medium-high severity wildfire in September 2012, different treatments with wheat straw <ins cite="mailto:Michele%20Francis" datetime="2015-01-23T16:03">were </ins>applied to the burnt soil in mulch strips (0.8 and 1 Mg ha<sup>-1</sup>) <del cite="mailto:Michele%20Francis" datetime="2015-01-23T16:03"></del><del cite="mailto:Michele%20Francis" datetime="2015-01-23T15:50"></del><ins cite="mailto:Michele%20Francis" datetime="2015-01-23T15:50">using </ins>quadruplicate <ins cite="mailto:Michele%20Francis" datetime="2015-01-23T15:51">10 m x 40 m </ins><ins cite="mailto:Michele%20Francis" datetime="2015-01-23T15:49">plots </ins><del cite="mailto:Michele%20Francis" datetime="2015-01-23T15:51"></del><del cite="mailto:Michele%20Francis" datetime="2015-01-23T15:49"></del>and compared with the corresponding burnt untreated control. Soil samples were collected from the A horizon (0-2.5 cm depth) at different sampling times <del cite="mailto:Michele%20Francis" datetime="2015-01-23T17:15"></del><ins cite="mailto:Michele%20Francis" datetime="2015-01-23T17:15">for 12 months</ins> after the wildfire<del cite="mailto:Michele%20Francis" datetime="2015-01-23T16:03"></del><ins cite="mailto:Michele%20Francis" datetime="2015-01-23T15:48">,</ins> and a wide range of physicochemical, chemical and biochemical soil properties (water retention, pH, electric conductivity, total C, <sup>13</sup>C, extractable C, water soluble C, soluble carbohydrates, total N, <sup>15</sup>N, microbial biomass C, soil respiration, bacterial activity, b-glucosidase, urease and phosphatase activities) were analyzed. The results showed that the application of straw mulch had a minor influence on the post-fire soil quality but, in contrast, the sampling time showed a significant influence attributed to short- and medium term changes in soil properties induced by both fire and climatic conditions.


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