施磷和培养时间对两种石灰性土壤无机磷形态转化的影响

采用培养试验研究了施磷和培养时间对两种石灰性土壤无机磷形态转化及其有效性的影响。结果表明:不施磷肥时,随着培养时间的延长,两种土壤各种无机磷均略有增加;施入不同数量磷肥后,两种土壤中各种无机形态磷均有不同程度的增加,但Ca2-P和Ca8-P在培养初期均急剧增加,而后Ca2-P逐渐下降,Ca8-P则为有增有减,Al-P、Fe-P、Ca10-P和O-P含量随培养时间呈持续增加趋势。     

雌禽就巢行为的调控

阐述了雌禽就巢行为产生的机理,介绍了调控雌禽就巢行为的4种方法:遗传调控法、环境调控法、免疫调控法和药物调控法,并展望了雌禽就巢行为研究的前景。     

N Dynamics under Reduced Tillage

Different methods of tillage are investigated in a field trial in Austria. In those variants where soils are treated with a cultivator respectively a plough in autumn the contents of mineral N (Nmin) in 0-90cm soil depth increased significantly. Therefore the danger of N-leaching or N-losses in autumn or winter is higher in intensively tilled soils (without plant cover) than in soils with minimum tillage (treatment only with rotary driller without any primary treatment before seeding). In this variant Nmin-contents are lower even at the beginning of vegetation due to the plant cover and reduced tillage. At this time the potential of N mineralisation is higher in the minimum tilled plots compared to the more intensively tilled soils due to the accumulation of organic matter. However, despite enhanced potential N availability the N contents of the crops did not increase. The yields don't differ in the investigated tillage systems and N balances are the highest under minimum tillage, therefore a higher N fertilisation in this variant cannot be recommended. An adaptation of N fertilisation according to the lower mineral N contents in spring should be investigated.     

不同氮源及秸秆添加对菜地土壤N_2O排放影响

在饱和田间持水量WFPS(water-filled pore space)为75%、温度为25℃的条件下,用室内培养研究设施菜地土壤在不同氮肥种类(硝酸钙CN,碳酸氢铵AB,硫酸铵AS,尿素U,对照CK)和有无秸秆添加情况下N2O的排放特征。培养17天的结果表明,各种肥料类型中,对照和硝态氮肥处理最先出现N2O排放高峰,铵态氮肥处理出现较晚。无论有无秸秆,碳酸氢铵(AB)处理的累积排放量都最高,分别为4.206±0.899和2.159±0.256μg g-1干土,铵态氮肥处理N2O排放量明显高于硝态氮肥。添加秸秆后各处理N2O排放明显增加,比未施秸秆增加1倍多(CN处理除外)。不同处理(CK除外)的N2O累积排放量与时间的关系都可用y=aLn(x)+b表示(P<0.001)。实验还发现,施用氮肥会导致土壤酸化,添加秸秆可改善土壤酸化现象。     

Release of sulphate, potassium, calcium and magnesium from spent mushroom compost under laboratory conditions

The release of sulphate-sulphur (SO₄ ^2–-S), potassium (K), calcium (Ca) and magnesium (Mg) from soil amended with spent mushroom compost (SMC), a by-product of mushroom production, was measured for 16 weeks in an open laboratory incubation at 25°C. Rates of application were up to 80 t ha^–1 moist SMC (0.84% SMC dry weight) both with and without inorganic fertilizer. The rates of nutrient application in the inorganic fertilizer were: 338 kg ha^–1 N, 100 kg ha^–1 of both phosphorus and K, and 114 kg ha^–1 S. SMC contains 1.7% K, 6.5% Ca, 0.4% Mg and 1.2% S (of which 87% is inorganic), and has a carbon:sulphur ratio of 26. The release of SO₄ ^2–-S was rapid, and was described using either a first or mixed order exponential equation, or (underestimated) by the CENTURY model. The release of K, Ca and Mg was initially rapid (first order) and then declined to a constant rate (zero order). Their release was also described using first/first order or first order/parabolic diffusion equations. Model parameters indicated the relative sizes of both readily releasable and recalcitrant nutrient pools. The recovery of SMC-supplied nutrients in the absence of fertilizer was 75–83% of the S, 40–45% of the K, 14–20% of the Ca and 43–66% of the Mg. When fertilizer was applied 33–45% of the S, 22–36% of the K, 12–24% of the Ca and –4 to 20% of the Mg that were supplied by the SMC and fertilizer were recovered in the leachate. The generally lower nutrient recovery when fertilizer was applied could have resulted from the incomplete recovery of fertilizer S and K, from soil fixation of applied nutrients, and from the lower pH following fertilizer application. Received: 3 April 1997     

Extractability of 15N-labeled corn-shoot tissue in a sandy and a clay soil by 0.01 MCaCl2 method in laboratory incubation experiments

Management of N fertilization depends not only on the mineral N measured at the beginning of the growing season but also on the status of the low-molecular-weight organic-N fraction. Our study was conducted to analyze how much of the ¹⁵N applied in labeled cornshoot tissue would be recovered in 0.01 M CaCl₂-extractable ¹⁵N fractions and wheter a decrease in the CaCl₂-extractable ¹⁵N fraction quantitatively followed the trend in net mineralization of the ¹⁵N applied in corn-shoot tissue during an incubation period. The effects of adding ¹⁵N-labeled young corn-shoot tissue to a sandy soil and a clay soil were investigated for 46 days in an aerobic incubation experiment at 25°C. The application of 80 mg N kg^-1 soil in the form of labeled corn-shoot tissue (24.62 mg ¹⁵N kg^-1 soil) resulted in a significant initial increase, followed by a decrease the labeled organic-N fraction in comparison with the untreated soils during the incubation. The labeled organic-N fraction was significantly higher in the sandy soil than in the clay soil until the 4th day of incubation. The decrease in labeled organic N in the sandy soil resulted in a subsequent increase in ¹⁵NO _inf3 ^sup- during the incubation. Ammonification of applied plant N resulted in a significant increase in the 1 M HCl-extractable non-exchangeable ¹⁵NH _inf4 ^sup+ fraction in the clay soik, owing to the vermiculite content. The ¹⁵N recovery was analyzed by the 0.01 M CaCl₂ extraction method; at the beginning of the incubation experiment, recovery was 37.0% in the sandy soil and 36.7% in the clay soil. After 46 days of incubation, recovery increased to 47.2 and 43.8% in the sandy and clay soils, respectively. Net mineralization of the ¹⁵N applied in corn-shoot tissue determined after the 46-day incubation was 6.60 mg ¹⁵N kg^-1 soil (=34.9% of the applied organic ¹⁵N) and 4.37 mg ¹⁵N kg^-1 soil (=23.1% of the applied organic ¹⁵N) in the sandy and the clay soils, respectively. The decrease in the labeled organic-N fraction extracted by 0.01 M CaCl₂ over the whole incubation period was 3.14 and 2.33 mg ¹⁵N kg^-1 soil in the sandy and clay soil, respectively. These results indicate that net mineralization of ¹⁵N was not consistent with the decrease in the labeled organic-N fraction. This may have been due to the inability of 0.01 M CaCl₂ to extract or desorb all of the applied organic ¹⁵N that was mineralized during the incubation period.     

Chaotic or deterministic development of nematode populations in pine forest humus incubated in the laboratory

Humus material from an old stand of Scots pine and from an open area clearcut 13–15 years ago was incubated in the laboratory. The incubations were started in different years and the differences in nematode faunal development between the years were compared with site characteristics. In all incubations there was an increase in total nematode abundance. The total number and diversity of nematodes were higher in humus from the forest than from the clearing. The results indicated that biotic control mechanisms were much weaker in the humus from the clearcut area, where a strong dominance of Acrobeloides nanus occurred in most incubations. The differences in faunal development between years were rather large. A certain pattern of unpredictability indicated that the nematode fauna was a rather labile component of the community of soil organisms in a pine forest soil.     

Comparison and improvement of methods for determining soil dehydrogenase activity by using triphenyltetrazolium chloride and iodonitrotetrazolium chloride

The triphenyltetrazolium chloride (TTC) method described by Thalmann (1968) and the iodonitrotetrazolium chloride (INT) method described by Spothelfer-Magaña and Thalmann (1992), used for measuring soil dehydrogenase activity, have been modified to overcome some methodical short-comings. Absorption maxima of 485 nm for triphenylformazan dissolved in acetone, 491 nm for iodonitrotetrazolium formazan (INTF) dissolved in tetrahydrofuran and 455 nm for INTF dissolved in N,N-dimethylformamide are recommended for measuring wavelengths. Extracting triphenylformazan twice with acetone is less toxic and proved to be at least as efficient as extraction with a mixture of 90% acetone and 10% carbon tetrachloride (Thalmann 1968 method). Tetrahydrofuran and dimethylformamide were equally good in extracting INTF from soils, but the former was less toxic. Anaerobic incubation resulted in the formation of higher amounts of triphenylformazan and INTF as well as reduced standard error. Both TTC and INT reduction showed high reproducibility and good differentiation of the microbial activity of six soils. For several reasons (more easily determined substrate dose depending on different soil types, better reduction, shorter incubation time), INT reduction seems to be a more suitable method of measuring soil microbial activity than TTC reduction.     

Testing the stability of carbon pools stored in tussock sedge meadows

Tussocks formed by Carex stricta are a relatively large carbon (C) pool in sedge meadows, but the stability of organic matter in these ecosystems is not well understood. We initiated year-long incubation experiments (22.5 °C) to evaluate the CO₂ and CH₄ production potentials of sedge meadow substrates under field moist and inundated treatments from five sites in the Upper Midwest, USA (4 reference, 1 restored). C mineralization potentials decreased with depth (tussocks > underlying soil), and were positively correlated with macro-organic matter content and negatively with lignin. Across sites, C stored in tussocks and soil at the restoration was the least stable, suggesting that the restoration of C-storage function may take decades. Mineralization potentials were similar between field moist and inundated treatments, but inundation resulted in higher methane production, accounting for 24–51% of total carbon mineralized from tussocks. In the field however, C. stricta tussocks emitted less methane (393 ± 76 mg CH₄ m⁻² d⁻¹) than tussock interspaces (1362 ± 371 mg CH₄ m⁻² d⁻¹) early in the growing season; we suggest that tussock tops oxidized methane produced from deeper anoxic horizons. Our results highlight the importance of considering how microtopography modulates greenhouse gas flux from wetlands and suggests that the C stored in the older, more decomposed C. stricta tussock sedge meadow substrates (both within and between sites) is relatively stable.     

Physicochemical changes in Mazafati date fruits incubated in hot acetic acid for accelerated ripening to prevent diseases and decay

A method was developed and optimized for the accelerated ripening of date fruits of cultivar ‘Mazafati’ to prevent diseases and decay. The date fruits were incubated in hot acetic acid solution 0.5% at 40 + 1 °C for 72 h. During the process some physicochemical changes in the fruits were studied and were found to be comparable with the changes in the fruits that naturally ripened on the tree. Fruit firmness, water insoluble solid (WIS), protein, pH, L*a*b* and E decreased during accelerated ripening whereas in control samples at 4 °C increased. Total solid (TS), total soluble solid (TSS) and acidity were slightly higher in treated fruits compared to control fruits. The greatest loss of fruit firmness occurred during the first 12 h of incubation. Organoleptic tests also showed little difference between the naturally ripened fruits on trees and accelerated ripened fruits in hot acetic acid. Overall there was no difference between the fruits and were readily acceptable to consumers.