Isotopic studies of the nitrogen balance in a cracking clay. II. Recovery of nitrate 15N added to columns of packed soil and microplots growing wheat in the field

Soil Research ◽  
1975 ◽  
Vol 13 (1) ◽  
pp. 53 ◽  
Author(s):  
ET Craswell ◽  
AE Martin
Keyword(s):  
Nitrogen Balance ◽  
Clay Soil ◽  
Heavy Rain ◽  
Plant Analysis ◽  
The Third ◽  
Isotopic Studies ◽  
Heavy Clay ◽  
Nitrate Fertilizer ◽  
Series Of Experiments

In a series of experiments, 15N-labelled nitrate fertilizer was used to study the nitrogen balance of a heavy clay soil. Two of the experiments employed 60-cm deep, 16-cm diameter columns of packed soil. In the first, no added 15N was lost until heavy rain saturated the soil in the undrained columns. Subsequently, fallow and planted columns lost 25% of the 15N added. While denitrification appeared primarily responsible for these losses, some of the 15N may have been lost by weathering of the plants during senescence. This experiment was repeated with precautions to prevent excessive rain saturating the soil. After 16 weeks, only 6 � 4.5% of the added 15N was not accounted for by soil and plant analysis. In the third experiment, I5N was added to 16-cm diameter confined microplots in situ. The microplots were fallow and were confined by 60-cm deep plastic pipe. After 16 weeks, during which 190 mm of rain fell, 97.7 � 2.4% of the added 15N was recovered.

Isotopic studies of the nitrogen balance in a cracking clay. I. Recovery of added nitrogen from soil and wheat in the glasshouse and gas lysimeter

Soil Research ◽  
1975 ◽  
Vol 13 (1) ◽  
pp. 43 ◽  
Author(s):  
ET Craswell ◽  
AE Martin
Keyword(s):  
Stable Isotope ◽  
Nitrogen Balance ◽  
Limit Of Detection ◽  
Complete Recovery ◽  
Nitrogen Fertilizers ◽  
Common Finding ◽  
Plant Analysis ◽  
Isotopic Studies ◽  
Fate Of Nitrogen ◽  
The Common

The stable isotope 15N was used to study the fate of nitrogen fertilizers applied to a black earth growing wheat. In a glasshouse experiment using soil packed at 56 % moisture (pF 2) into pots, added nitrate was almost completely recovered (mean, 98.8 � 2.3 %) by soil and plant analysis. This experiment was repeated using 15N-labelled ammonium as well as nitrate; mean recoveries at 15 weeks were 96.8 and 97% respectively (� 2.2% at P < 0.05). A series of pots with soil wetter than pF 2 (at 63% moisture) was also included in an attempt to favour denitrification. Again, virtually complete recovery of added 15N was measured, 97 and 96.8% at 56 and 63% moisture respectively. Fallow and planted systems were then studied in a gas lysimeter. During experiments lasting up to 14 weeks, gaseous losses as 15N-labelled denitrification products were less than the equivalent of 0.2 �g nitrogen/g soil (the lower limit of detection with a mass spectrometer). Although analysis of plant and soil from the lysimeter in two experiments showed virtually quantitative recovery (99.7 and 97.05%), small (0.16%) losses of labelled ammonia into the lysimeter atmosphere were detected. The significance of these results is discussed in relation to the common finding of large deficits in nitrogen balance studies.

Effect of soil type on nitrogen balance at maturity in wheat characterized using 15N-labelled NH4 NO3-fertilizer and sink - source modifications at flowering

1998 ◽  
Vol 25 (4) ◽  
pp. 475
Author(s):  
Lynda Hannachi ◽  
Agnès Bousser ◽  
Eliane Deléens
Keyword(s):  
Nitrogen Balance ◽  
Flag Leaf ◽  
Grain Filling ◽  
Soil Nitrate ◽  
Loamy Soil ◽  
Split Dose ◽  
The Third ◽  
Initial Soil ◽  
Nitrate Fertilizer ◽  
Fertilizer Recovery

Wheat plants were grown in a greenhouse in containers filled with chalky or loamy soil. Single-labelled ammonium nitrate fertilizer NH415NO3 or 15NH4 NO3 (5 atom% 15N) was applied in a split-dose after the third leaf-stage. Initial soil nitrate levels were lower in chalky soil. At maturity, the amount of N recovered in shoots was lower in chalky plants (CP) than in loamy plants (LP) but N fertilizer recovery was higher in CP than in LP. There was a greater 15NO3 recovery, in CP: 15NO3 / 15NH4 being 1 in LP and 1.3 in CP seeds. This was explained by efficient N mobilization enriched in 15NO3 in CP. Leaf excision or shoot shading at flowering changed the seed 15NO3 / 15NH4 ratio; it increased in CP and decreased in LP for plants with excised leaves whereas it was not modified in CP but decreased in LP for shaded plants. This indicated that grain filling was predominantly via mobilization in CP, whereas a late assimilation was involved in LP. The flag leaf in CP was the site for early and transient storage of NO3- and later a main source of assimilated N for seeds. Benefits previously observed in vegetative wheat plants grown on chalky soils compared to loamy soils with respect to enhanced NO3 utilisation, are also manifest at grain-filling and maturity.

57Fe Mössbauer Spectroscopic Study of the Geometrical Effects In the Catalytic Reactions with Intercalation Compounds

1982 ◽  
Vol 20 ◽  
Author(s):  
P.P. Vaishnava ◽  
P.A. Montano
Keyword(s):  
Ferric Chloride ◽  
Catalytic Reactions ◽  
Fischer Tropsch ◽  
Reaction Conditions ◽  
Intercalated Graphite ◽  
The Third ◽  
Intercalated Compounds ◽  
Catalytic Sites ◽  
Geometrical Effects

ABSTRACTIn situ 57Fe Mössbauer spectra are reported for the first-, higher-stage ferric chloride, and a mixed ferric chloride-potassium chloride intercalated graphite catalysts under reduction and Fischer-Tropsch reaction conditions. The mass spectroscopic measurements reveal a different catalytic selectivity for the three catalysts. The first two catalysts predominantly possess a higher selectivity for methane, whereas the third catalyst has higher selectivity for the formation of propane. The differences are attributed to geometrical effects in the catalytic sites of the intercalated compounds.

scholarly journals Effect of Yeast-Fermented Citrus Pulp as a Protein Source on Nutrient Intake, Digestibility, Nitrogen Balance and In Situ Digestion Kinetics in Nili Ravi Buffalo Bulls

Animals ◽  
2021 ◽  
Vol 11 (6) ◽  
pp. 1713
Author(s):  
Muhammad Awais ◽  
Muhammad Sharif ◽  
Khurram Ashfaq ◽  
Amjad Islam Aqib ◽  
Muhammad Saeed ◽  
...  
Keyword(s):  
Nitrogen Balance ◽  
Nutrient Intake ◽  
Dry Matter ◽  
Experimental Period ◽  
Nutrient Digestibility ◽  
Protein Source ◽  
Cell Protein ◽  
Citrus Pulp ◽  
Digestion Kinetics

A study was carried out to evaluate the effect of single cell protein (SCP) supplement as a protein source on nutrient intake, digestibility, nitrogen balance and in situ digestion kinetics in four Nili Ravi buffalo bulls. Four iso-caloric and iso-nitrogenous concentrates containing 3, 6, 9 and 12% of Saccharomyces cerevisiae-fermented citrus pulp were formulated. All animals were fed a ration with a concentrate/forage ratio of 50:50. Diets were provided ad libitum twice a day as a total mixed ration in a 4 × 4 Latin Square Design. Each experimental period lasted 3 weeks while the overall study 12 weeks. The first 2 weeks of each experimental period were used as adaptation period while the third week as collection period. Chemical composition of fermented citrus pulp appeared as an excellent source of protein. No significant difference was observed on dry matter intake, digestibility of nutrients and SCP among all the treatments. Moreover, no significant effect was observed on ruminal pH and ammonia nitrogen at different times. Rate of disappearance and lag time of in situ dry matter digestion kinetics remained nonsignificant regardless of SCP percentage. Based on results of similar nutrients intake, nutrient digestibility, and ruminal parameters it is concluded that SCP could be used in the concentrate diet of ruminant up to 12%. Furthermore, the SCP has the potential of an alternative protein source in animal diet formulation.

Investigation into the effect of tillage on solute movement to drains through a heavy clay soil

2006 ◽  
Vol 15 (2) ◽  
pp. 94-100 ◽  
Author(s):  
C.D. Brown ◽  
V.L. Marshall ◽  
A. Deas ◽  
A.D. Carter ◽  
D. Arnold ◽  
...  
Keyword(s):  
Clay Soil ◽  
Heavy Clay ◽  
Solute Movement

Investigations in crop husbandry. III. Effect of time of application of sulphate of ammonia to wheat

1936 ◽  
Vol 26 (2) ◽  
pp. 316-327 ◽  
Author(s):  
F. H. Garner ◽  
H. G. Sanders
Keyword(s):  
Field Experiments ◽  
Clay Soil ◽  
Foot Rot ◽  
Plant Establishment ◽  
Poor Condition ◽  
Time Of Application ◽  
Gravelly Soil ◽  
Heavy Clay ◽  
Crop Husbandry

1. Over a period of six years seven field experiments were carried out to study the effect of the time of application of sulphate of ammonia to autumn-sown wheat.2. Three experiments were located on light gravelly soil which had been farmed highly for some years, and in those three cases sulphate of ammonia decreased yield, irrespective of time of application; the reduction in yield was of the order of 10 per cent. and is ascribed to more lodging and greater incidence of “foot-rot”.3. Three experiments were located on heavy clay soil in poor condition; in these sulphate of ammonia gave percentage increases in yield of 18, 20 and 7.4. Evidence is produced that early dressings of sulphate of ammonia do not affect germination or plant establishment, but that they tend to increase tiller formation by the end of February.

scholarly journals Reclamation of a Saline-Sodic Soil by Use of Molasses and Distillery Slops

1969 ◽  
Vol 50 (3) ◽  
pp. 209-217
Author(s):  
Raúl Pérez Escolar
Keyword(s):  
Puerto Rico ◽  
Organic Acids ◽  
Clay Soil ◽  
Mass Action ◽  
Soil Reclamation ◽  
Exchangeable Sodium ◽  
Dry Period ◽  
Action Effect ◽  
Saturation Extract ◽  
Heavy Clay

Data are presented on a laboratory study conducted to determine the effects of the use of blackstrap molasses and rum distillery slops on the reclamation of a highly saline-alkali heavy clay soil of southwestern Puerto Rico. The study revealed that even the lowest levels of distillery slops and diluted molasses, around 2.3 acre-inch, were sufficient to lower the conductivity of the soil-saturation extract from 67 mmhos/cm. to less than 3, and the exchangeable sodium percentage from 43 to less than 1 percent. It is believed that most of the Ca and Mg found in leachates of columns treated with the most slops or molasses may be attributed to the production of organic acids during the decomposition of slops and molasses. These organic acids rendered soluble the soil-free CaCO3 and MgCO3, widening the Ca and Mg:Na ratio to substitute the sodium by a mass action effect. Subjecting the soil to a dry period in between, the 6 and 7 acre-feet of water did not alter the movement of water and resulted in a complete soil reclamation.

scholarly journals Preliminary Report on a Stratified Late Archaic-Woodland Era Rockshelter in Rogers County, Oklahoma

1995 ◽  
Author(s):  
Robert W. Jobson ◽  
Frank Winchell ◽  
A.E. Picarella ◽  
Kiven C. Hill
Keyword(s):  
Clay Soil ◽  
Woodland Period ◽  
Soil Horizon ◽  
Late Archaic ◽  
Human Skeletal Remains ◽  
Early Woodland ◽  
Time Period ◽  
Archeological Evidence ◽  
Preliminary Description

In northeastern Oklahoma, very little is known about the transition from the Late Archaic to the Woodland period (Wyckoff and Brooks, 1983: 55). To date, most of the archeological evidence documenting this time period has been derived from sites with mixed or otherwise uncertain components. In this report, we present a preliminary description of a small rockshelter, 34RO252, which has a Late Archaic deposit stratigraphically below a Woodland era cultural deposit. These two deposits are unmixed, discrete, and are physically separated by an apparently sterile clay soil horizon. It is anticipated that the stratified cultural deposits at this site will help characterize the transition from the Late Archaic to the Early Woodland period along the Verdigris River in northeast Oklahoma. This site was first reported in April 1994 by two men who had discovered partially exposed human skeletal remains located in the rear remnant of a rockshelter at Oologah Lake in Rogers County, Oklahoma. The two men illegally excavated the remains and removed them from the site. 1 The rockshelter where the remains originated was subsequently examined by the authors and additional skeletal material was identified, in situ, in an exposed soil profile. A series of three radiocarbon assays, described below, placed the cultural deposit and the human remains within the Late Archaic-Woodland period (circa 780 B.C. to A.O. 900).2 This site is provisionally classified as corresponding to a cultural sequence that includes the old Grove C described by Purrington and Vehik.

scholarly journals Surface irrigation with saline water on a heavy clay soil in the Medjerda Valley, Tunisia.

1967 ◽  
Vol 15 (4) ◽  
pp. 281-303
Author(s):  
J.A. Van 't Leven ◽  
M.A. Haddad
Keyword(s):  
Electrical Conductivity ◽  
Clay Soil ◽  
Saline Water ◽  
Surface Irrigation ◽  
Soil Extracts ◽  
Fallow Period ◽  
Salinity Effects ◽  
Heavy Clay ◽  
Winter Crops ◽  
Resting Period

On a clay soil rich in lime, with drain spacings of 30 and 60 m, one section (A) after four crops of artichokes over a two-year period, with fairly intensive irrigation with saline water (approx 700 mm annually) showed no harmful salinity effects; in the upper 120 cm the electrical conductivity of soil extracts (EC) seldom exceeded five. On section B, with well-distributed irrigation, which was not intensive except for tomatoes in one summer, salinity was fairly uniform in the profile (EC 4-6). In section C, under continuous lucerne and with 1000-1200 mm water annually, salinity increased, especially with depth, and a fallow period was needed. In section D, under four artichoke crops followed by maize, with more intensive irrigation than in A and B, EC of the 80-120 cm layer was 7-8, and maize growth was retarded slightly. In addition to fallowing, the inclusion in rotations of winter crops and of perennials with a resting period in summer, e.g. artichokes, is recommended. A drain spacing of 60 m was adequate. (Abstract retrieved from CAB Abstracts by CABI’s permission)

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