Long-term effects of straw and farmyard manure on crop yields and soil properties

The effect of cereal straw with added mineral N fertilization on crop yields, N uptake, total organic C content and hot water soluble C content in topsoil and on the relationships between organic C content in topsoil and organic matter balance was evaluated in a long-term field experiment established in 1966. The effect of straw plus mineral N fertilization was similar to the effect of farmyard manure (FYM) in the dry matter yields and also in the N uptake by plants. The effect of straw and mineral N fertilization on the organic C accumulation in soil was inferior to the effect of farmyard manure. Relationships between organic matter balance and total organic C content in the topsoil was positive and statistically significant. A favourable effect of mineral NPK fertilization on the C sequestration to soil was related to the effect of FYM fertilization.     

Nachhaltige Bodennutzung,gemessen am Ertrag sowie an C‐ und N‐Bilanzen

Der Boden gehört zu den wichtigsten Lebensgrundlagen des Menschen, die Erhaltung seiner Fruchtbarkeit ist deshalb unerläßlich. Am Beispiel ausgewählter Prüfglieder des Statischen Düngungsversuches Bad Lauchstädt wird nach 90 Versuchsjahren der Einfluß unterschiedlicher Düngung (ohne, mineralisch, organisch und organisch/mineralisch) auf die Nachhaltigkeit der Bodennutzung, gemessen am Winterweizenertrag, Zuckerertrag sowie an C‐ und N‐Bilanzen dargestellt und im Zusammenhang mit den Begriffen Bodenfruchtbarkeit und Bodengesundheit diskutiert. Die ausschließliche Mineraldüngung bringt auf diesem Standort (Lößschwarzerde) bei beiden Fruchtarten keine geringeren Erträge als die kombinierte Düngung, verursacht die geringsten N‐Verluste und schneidet auch beim Vergleich der C‐Bilanzen am günstigsten ab. Es wird geschlußfolgert, daß mit der Erzeugung von Biomasse zur Energie‐ und Rohstoffgewinnung ein Beitrag zur Verringerung der energiebedingten CO₂‐Emmission geleistet werden kann und eine umsichtige, den gegenwärtigen Kenntnisstand berück‐sichtigende Mineraldüngung diesen Prozeß positiv beeinflußt. Ziel sollte sein, nicht nur einen geringen Anteil der Nutzfläche alternativ zu bewirtschaften, sondern die gesamte Landwirtschaft leistungsfähig, ökologisch vertretbar und ökonomisch zu gestalten.     

长期施肥对潮土团聚体有机碳分子结构的影响

采取长期施用有机肥（CM）、一半化肥氮和一半有机肥氮（HCM）、化肥（NPK）和不施肥对照（CK）的土壤,用湿筛法分为大团聚体（2000~250 μm）、微团聚体（250~53 μm）和粉砂 黏粒组分（<53 μm）,利用固态13C-核磁共振技术分析了土壤和团聚体中有机质的分子结构特征。结果表明,随着团聚体粒径减小,烷基碳/烷氧碳比值逐渐提高,并与土壤C/N呈显著负相关（R2 = 0.421,p = 0.022）,表明随着团聚体粒径减小,有机质的分解程度不断增加。与对照土壤相比,长期施用有机肥（HCM和CM处理）提高了土壤中烷氧碳和羰基碳的相对含量,烷氧碳的增加主要是由于大团聚体中甲氧基和含氮烷基碳相对含量的增加,羰基碳则主要在大团聚体和微团聚体中积聚。施用化肥土壤提高了烷氧碳和烷基碳的相对含量,烷氧碳增加主要是由于大团聚体中甲氧基和含氮烷基碳以及微团聚体中含氧烷基碳相对含量的提高,烷基碳增加主要发生在大团聚体。有机肥和化肥处理土壤中芳基碳相对含量降低1.8%~4.6%,主要是大团聚体和微团聚体中芳基碳比例下降引起的。而在粉砂 黏粒组分中芳基碳和酚基碳均增加,烷基碳相对含量降低5.9%~7.1%,表明施肥更利于芳香碳在小粒径组分中积累,减弱烷基碳在小粒径组分中的积累。结果表明长期施用有机肥可通过大团聚体和微团聚体物理保护肥料带入的大量碳水化合物和有机酸从而提高土壤有机碳含量。     

Fate of humic acids isolated from natural humic substances

Composition of humic acids (HA) is a function of plant-derived inputs, degradation processes regulated by microorganisms, organo-mineral interactions and age. Characterization of different origin humic substances is important for evaluation of their contribution to stabile and labile carbon pool in the environment. The relative abundance of chemical components in HA isolated from soils, compost, commercial lignohumates, alginite, acadiane and lignite was studied with aim to quantify content of important biomarkers such as amino acid, lipids and polyphenols. HA were considered as a heterogeneous complex and high concentration of peptides, polyphenols and lipids was determined in acadian-HA to compare with soil-HA. Compost-HA contained much more amino acids to compare with soil-HA samples. Alginite-HA and lignite-HA were similar in biomarkers content to soil-HA. Fourier transform infrared spectroscopy confirmed that chemical composition and functional groups content differs with the origin, humification degree and the age of studied samples. Soil-HA are typically composed of a variety of ?OH, COOH?, C–O, C–H₂, (aliphatic and aromatic) groups, quinines, lignin fragments, polysaccharide, monosaccharide and proteins fragments, which are linked together by ?O?, ?NH?, ?H=, >C=O, metal ions and –S? groups. ¹³C NMR spectroscopy showed that aromatic carbon content was the highest in lignite-HA and soil-HA.     

Effect of Daylength on the Nitrogen Status of Timothy (Phleum pratense L.)

Abstract

In two experiments timothy plants (Phleum pratense L., cultivars ‘Bodin’ and ‘Grindstad’, well established and vernalized in the first experiment and 7 weeks old in the second) were given daylength treatments with 12 h of photosynthetically active radiation (PAR) and day-lengthening light of low irradiance for from 2 to 13 weeks. Significant daylength effects on dry-matter, total nitrogen, nitrate and soluble protein content in the leaves of plants were demonstrated after only two weeks of treatment. The nitrogen and protein content decreased with increasing daylength, irrespective of the developmental stage of the plants. The dry-matter content increased with daylength when long days had induced generative development and decreased when all treatments at the same harvest were vegetative. The total nitrogen and protein per plant did not decrease from short to long days. The lower nitrogen and protein content in long days can therefore be regarded as a dilution caused by the increased dry-matter production found in these treatments. The observed effects of daylength on the ratio of assimilated nitrogen to assimilated carbon might be direct or indirect, since long days induce both enhanced dry-matter production and generative development in Bodin and Grindstad.     

Qualitative modifications of humic acid-like and core-humic acid-like during high-rate composting of pig faeces amended with wheat straw

Humic acid-like (HA-like) and core-humic acid-like (core-HA-like) were characterized during the high-rate composting process by CP-MAS ¹³C NMR, pyrolysis-gas chromatography (GC)/mass spectrometry (MS), and elemental analysis. Results obtained indicated that humification proceeded through a relative concentration of aromatic fractions due to the faster degradation of the O-alkyl and alkyl fractions. Core-HA-like, after purification of the parent material, showed a large reduction of the O-alkyl fraction in terms of HA-like. We concluded that HA-like consisted of refractory organic molecules, such as lignin and biopolymers, which formed a stable structure (core-HA-like) coated with degradable material associated with the core by weak physical association, ether or ester bounds.     

Evolution and qualitative modifications of humin-like matter during high rate composting of pig faeces amended with wheat straw

During a 4-week period of composting of wheat straw-amended pig faeces, humin (HU)- and core-HU-like matter were isolated by NaOH-Na₄P₂O₇ treatment of the compost bed, respectively, without and with previous extraction by organic solvent and by H₂SO₄. The changes in the content and elemental composition of both fractions in the compost bed were monitored. Evidence of the compositional changes was also obtained by NMR spectroscopy and by pyrolysis-GC / MS studies. The results indicated that core-HU-like matter was mainly aromatic, while HU contained both core-HU-like and other types of easily degradable organic matter. Correlation of the data found in this study with data from previous studies on humic acid (HA)- and core-HA-like matter in the same composting process indicated that in the time range from 2 to 4 weeks, the weight loss of the core-HU-like matter amounted to 788 g, whereas the weight of total core-HA-like matter increased by 87 g. In spite of the high weight loss, the NMR and pyrolysis-GC / MS spectra failed to reveal significant changes in the chemical nature of the core-HU-like residue. However, the chemical composition of the core-HA-like matter changed significantly and tended to become similar to that of the core-HU-like matter when the composting time increased. The data suggest that, during composting, core-HU-like matter undergoes both conversion to new core-HA-like soluble matter and biodegradation to volatile products.     

CH4 production potential in a paddy soil exposed to atmospheric CO2 enrichment

Abstract

An anaerobic incubation experiment was conducted to investigate methane (CH₄) production potential in soil samples collected from a paddy field after exposure to free-air CO₂ enrichment (FACE). The FACE experiment with two CO₂ levels, ambient and ambient + 200 p.p.m.v CO₂ during the rice growing season, was conducted at Shizukuishi, Iwate Prefecture, Japan. The soil was a wet Andosol. Soil samples were taken from the surface (0–1 cm) and the sub-surface (1–10 cm) soil layers 2 months after rice harvest. Sub-samples of the fresh soils were put into glass bottles and submerged under N₂ gas headspace during the incubation. The results showed that, prior to incubation, the contents of total C and dissolved organic C (DOC) were significantly greater in FACE soil than ambient soil. During the incubation, CH₄ production potential was approximately 2–4-fold higher in FACE soil than ambient soil and approximately 500–1,000-fold greater in surface soil than sub-surface soil. In general, the FACE soil contained more DOC than ambient soil, particularly in the surface soil layer. These findings suggest that FACE treatment exerted long-term positive effects on CH₄ production and increased organic C content in this paddy soil, particularly in the surface soil layer.     

An examination of the total analysis of major elements in soil samples

Recently conventional chemical analyses were mostly replaced by instrumental analysis. Although results from both methods were examined in details after the samples had been solubilized or extracted by appropriate techniques, the solubilization method was considerably altered so as to be convenient for the following analysis. In atomic absorption spectrophotometry (AAS), for example, fusion technique was mostly inadequate because of the higher salts concentration in the obtained solution. The use of H₂SO₄ must also be avoided in acid digestion for SO₄ ^2- precipitates with Sr²⁺ or La³⁺ which must be added to eliminate interferences in the succeeding procedure. Therefore, it is essential to consider the whole scheme including sample treatments to evaluate the suitability of instrumental analysis. In this experiment, the suitability of the methods which have been employed in our laboratory was examined by analyzing 9 rock standards.     

Changes in proline-14C metabolism in barley seedlings germinating at low temperature

Changes in the metabolic pattern of proline-¹⁴C were examined in barley seedlings germinated at the low temperature of 2°C (LT) and compared with those germinated at 25°C (HT). In the LT shoots. proline-¹⁴C incorporation was higher in the cationic fraction and lower in the acid-neutral fraction than that of HT, respectively. More proline-¹⁴C of LT was converted to other amino acids, especially to acidic amino acids in free amino acid state, than was the HT proline-¹⁴C which had a comparatively wide distribution.

In the LT protein fractions. more proline-¹⁴C was incorporated into the cytoplasmic protein than into the cell wall protein. On the contrary, the radioactivity of the lIT cell wall increased more distinctively. proline-¹⁴C in the two proteins of LT was a little less converted to other amino acids than in those of HT. A little higher radioactivity was found in the aspartate and glutamate of the LT protein hydrolysates. The hydroxyproline which is closely related with proline had a little lower level of radioactivity in the LT cell wall.