Phosphorus release from cattle manure ash as soil amendment in laboratory-scale tests

ABSTRACT

Excessive application of animal manure to farmland leads to phosphorus (P) loss into the surrounding water. Manure is incinerated to convert it to P-rich ash as a slow-release P fertilizer. However, the potential P loss and P availability for plants from cattle manure ash (CMA) have not been fully understood. The aims of this study were to determine the P release mechanism from CMA and to propose appropriate application rates that mitigate P loss and increase available P to soil in Fukushima, where the soil is deficient in nutrients after the replacement of cesium-137-contaminated soil with sandy mountain soil. Different P fractions in CMA were sequentially extracted with H₂O, 0.5 M NaHCO₃, 0.1 M NaOH, and 1 M HCl. Phosphorus contents in different fractions of CMA were in the order of HCl–P > NaHCO₃–P > H₂O–P > NaOH–P. Water-soluble P release of CMA was also determined by kinetic experiments for 120 h. Results showed that total water-soluble P accounted for a maximum of 2.9% of total P in CMA over 120 h due to recalcitrant P compounds formed through incineration. The Fukushima sandy soil amended with CMA at three application rates, 94, 157, and 314 mg P kg^?1 (corresponding to 300, 500, 1000 kg P₂O₅ ha^?1) was incubated for 56 days. Cattle manure compost and KH₂PO₄ were applied at 157 mg P kg^?1 for comparison. Phosphorus release in water and CaCl₂ solution from ash-amended soil was significantly lower than those from compost and KH₂PO₄-amended soil at the same P application rate of 157 mg P kg^?1 (p < 0.05). Available P in ash-amended soil, determined by Fe-oxide impregnated strips, was not significantly different from those in compost-amended soil after day 7 and KH₂PO₄-amended soil on day 56 at the same P application rate. Thus, CMA reduces P losses from soil to the surrounding water while it increases P availability for plants. In comparison of different rates of CMA, P release in water or CaCl₂ was significantly greater at 314 mg P kg^?1 than at 94 or 157 mg P kg^?1, while the percentage of available P to total P was the lowest at the highest application rate (p < 0.05), suggesting that the best application rates were 94 and 157 mg P kg^?1 in this experiment.     

Factors Influencing the Determination of Microbial Biomass-Nitrogen in Submerged Soil

In a previous paper (1), a modification of the chloroform fumigation method (2) was proposed for estimating microbial biomass-nitrogen (N) in submerged soil. It was found that a large part of the living bacteria in the submerged soil was killed within about 12 h of the fumigation and was actively mineralized by subsequent anaerobic incubation.

In this paper, the following factors which influence the estimated amount of microbial biomass-N were examined: a) inoculation to fumigated soil, b) duration of anaerobic incubation, c) storage and sieving pretreatments of soil, and d) effect of fumigation on soil organic matter.     

Development of an enzyme-linked immunosorbent assay (ELISA) for residue analysis of the fungicide azoxystrobin in agricultural products

A direct competitive enzyme-linked immunosorbent assay (dc-ELISA) was developed for residue analysis of azoxystrobin in garden crops, for which the maximum residue limits (MRLs) are 0.5-50 mg/kg in Japan. For hapten synthesis, an ethyl carboxyl group was introduced to the 4-position of the 2-cyanophenoxy group in azoxystrobin, and its cyano group was changed to a methyl group. An anti-azoxystrobin monoclonal antibody was prepared from mice immunized with hapten-keyhole limpet hemocyanin conjugate. The dc-ELISA using prepared antibody showed 50-250-fold higher sensitivity compared to the MRLs. The working range of the dc-ELISA was 10-200 ng/mL. The dc-ELISA showed high specificity to azoxystrobin. When methanol extracts from nine kinds of garden crops spiked with azoxystrobin ranging near the MRLs were analyzed, the determined results by the dc-ELISA agreed well with the results of their controls. In addition, azoxystrobin spiked in garden crops homogenates was satisfactorily extracted by methanol solution and easily analyzed. The recovery rate of dc-ELISA was 96-109% and correlated well with the results obtained by HPLC analysis.     

Ethylene oxidation,atmospheric methane consumption,and ammonium oxidation in temperate volcanic forest soils

Temperate volcanic forest surface soils under different forest stands (e.g., Pinus sylvestris L., Cryptomeria japonica, and Quercus serrata) were sampled to study the kinetics of ethylene (C₂H₄) oxidation and the C₂H₄ concentrations that effectively inhibit oxidation of atmospheric methane (CH₄) and nitrification. The kinetics of C₂H₄ oxidation in temperate volcanic forest soils was biphasic, indicating that at least two different microbial populations, one with low and another with high apparent K _m values, were responsible for ethylene oxidation. Methane consumption activity and ammonium oxidation of soil were inhibited by adding ethylene. Added C₂H₄ at concentrations of 3, 10, and 20 μl C₂H₄ per liter in the headspace gas respectively reduced by 20%, 50%, and 100% atmospheric CH₄ consumption by soil, and these values were much smaller than those inhibiting ammonium oxidation in these forest soils; thus, the CH₄ consumption activity was more sensitive to the addition of C₂H₄ than ammonium oxidation. Previous studies have shown that accumulation of C₂H₄ in such volcanic forest soils within 3 days of aerobic and anaerobic incubations can reach a range from 0.2 to 0.3 and from 1.0 to 3.0 μl C₂H₄ per liter in the headspace gas, respectively. It is suggested that C₂H₄ production beneath forest floors, particularly after heavy rain, can to some extent affect the capacity of forest surface soils to consume atmospheric CH₄, but probably, it has no impact on ammonium oxidation.     

Effect of Biogas Digested Liquid on CH4 and N2O Flux in Paddy Ecosystem

Biogas production generates digested slurry as a byproduct. It can be used as a fertilizer especially after its conversion into digested liquid. A pot based study was conducted in order to evaluate the effect of the application of digested liquid on CH₄ and N₂O flux, and plant biomass in paddy. Analysis revealed that digested liquid treated soils released more CH₄ compared to ammonium sulphate and the control. Ammonium sulphate treated soil emitted the highest N₂O whereas digested liquid application decreased its emission significantly. Further, the cumulative emission over 101 d of the experiment was found to be higher for CH₄ (16.9 to 29.9 g m⁻²) compared to N₂O (−49.3 to 18.9 mg m⁻²) for all treatments. Digested liquid application had positive impact on plant variables such as panicle number and weight of panicles. This study suggests that digested liquid application significantly decrease N₂O emission and increase CH₄ emission possibly due to affecting the availability of organic C in the soil to microbial activity for methanogenesis. Another possibility for enhancing CH₄ emission by following biogas digested liquid could be attributed to the increase in plant biomass.     

Identification of QTLs for fruit quality traits in Japanese apples: QTLs for early ripening are tightly related to preharvest fruit drop

Many important apple (Malus × domestica Borkh.) fruit quality traits are regulated by multiple genes, and more information about quantitative trait loci (QTLs) for these traits is required for marker-assisted selection. In this study, we constructed genetic linkage maps of the Japanese apple cultivars ‘Orin’ and ‘Akane’ using F₁ seedlings derived from a cross between these cultivars. The ‘Orin’ map consisted of 251 loci covering 17 linkage groups (LGs; total length 1095.3 cM), and the ‘Akane’ map consisted of 291 loci covering 18 LGs (total length 1098.2 cM). We performed QTL analysis for 16 important traits, and found that four QTLs related to harvest time explained about 70% of genetic variation, and these will be useful for marker-assisted selection. The QTL for early harvest time in LG15 was located very close to the QTL for preharvest fruit drop. The QTL for skin color depth was located around the position of MYB1 in LG9, which suggested that alleles harbored by ‘Akane’ are regulating red color depth with different degrees of effect. We also analyzed soluble solids and sugar component contents, and found that a QTL for soluble solids content in LG16 could be explained by the amount of sorbitol and fructose.     

Changes in the coagulation parameters in dogs with protein-losing enteropathy between before and after treatment

Protein-losing enteropathy (PLE) is known to induce hypercoagulability and resultant thromboembolism in dogs. We hypothesized that hypercoagulability would improve if remission was obtained in dogs with PLE after treatment. This study aimed to evaluate the changes in the coagulation parameters after treatment in dogs diagnosed with PLE. As coagulation parameters, prothrombin time (PT), activated partial thromboplastin time (aPTT), fibrinogen, thrombin-antithrombin complex (TAT), D-dimer, and antithrombin (AT) were measured. In addition to these parameters, rotational thromboelastometry (ROTEM), which evaluates the comprehensive coagulation and fibrinolysis reactions of whole blood, was conducted and the data of clotting time (CT), clot formation time (CFT), α angle (α), maximum clot firmness (MCF) and lysis index at 60 min (LI60) were obtained. Eleven of the 14 dogs diagnosed with PLE were classified as responders to the treatment based on the changes in their plasma albumin (ALB) concentration after treatment. Significant increase in CFT and decrease of α and MCF indicating the resolution of hypercoagulability were found after treatment in responder dogs; however, there was no significant change in the coagulation and fibrinolysis parameters other than those measured by ROTEM. This study demonstrated that the hypercoagulability detected by ROTEM was significantly improved after treatment in dogs with PLE.     

水分管理对水稻生长期N2O排放的影响

通过温室盆栽试验研究相同施肥条件下,不同水分管理(持续淹水,分蘖肥后提前烤田、正常烤田和推迟烤田)对水稻生长期N2O排放的影响。结果表明,整个水稻生长期N2O的排放集中在施分蘖肥后的烤田期间及随后复水的5~8天内。在此期间各处理N2O排放量占季节排放总量的70.30%~94.26%;烤田前淹水及后期干湿交替阶段有少量N2O排放。对持续淹水处理而言,N2O的排放通量是正常烤田处理的12.10%。提前烤田、正常烤田和推迟烤田的平均N2O排放通量分别为188.56、158.48和147.84μg/(m2?h),随着烤田开始时间的推迟,N2O排放量逐渐减少。     

Emissions of nitrous oxide and methane from rice field after granulated urea application with nitrification inhibitors and zeolite under different water managements

Paddy and Water Environment - A field experiment was carried out to determine the emissions of nitrous oxide (N2O) and methane (CH4) and yield of rice grains under water management of continuously...