Phytotoxizität von Thallium (TI) in Hydrokultur Teil2: Einfluß von TI(III) auf das Wachstum und die Schwermetallgehalte von Erbsen- und Ackerbohnenpflanzen

Phytotoxicity of Thallium (Tl) in Culture Solution Part 2: Effects of Tl(III) on the Growth and Heavy Metal Contents of Pea and Field Bean Plants The effects of Tl(NO₃)₃ and Tl(III)EDTA on growth and heavy metal contents of pea plants (Pisum sativum L. cv. Aromata) and field bean plants (Vicia faba L. cv. Hangdown) were compared in hydroponic culture experiments. In the presence of Tl(NO₃)₃, the essential heavy metals were available to the plants in their ionic forms. When Tl(III)EDTA was present the essential heavy metals were available as chelated complexes. Dry matter production of the pea plants was inhibited to a greater extent by TI(II1)EDTA than by Tl(NO₃)₃. The distribution of TI within the plant was unaffected by the accompanying anion, however an increase of the TI content of the stems and the leaves was observed in the presence of TI(II1)EDTA. The micronutrients exhibited different interactions with TI(II1). In the presence of increasing concentrations of Tl(NO₃)₃ the Mn content of each organ and the Zn content of the roots were lowered, but the Zn content of the stems was increased. Increasing concentrations of TI(II1)EDTA resulted only in a decrease of the Mn content of the roots, but in an increase of the contents of Fe and Mn within the stems, and Fe, Mn, Zn, and Cu within the leaves. The increases may be due to concentration by growth inhibition. In contrast to pea plants, growth of field bean plants was inhibited only by TI(N03)). The field bean plants retained most of the TI within the roots independent of the TI compound in the solution. Chelation of TI(II1) resulted in higher TI contents of both the roots and the stems, but equal or reduced TI contents of the leaves. Whereas increasing concentrations of Tl(NO₃)₃ reduced the Mn content of each organ as well as the Zn content of the roots and the leaves, TI(II1)EDTA only reduced the Mn content of the roots.     

Plant lignin and nitrogen contents control carbon dioxide production and nitrogen mineralization in soils incubated with Bt and non-Bt corn residues

Bt (Bacillus thuringiensis) corn is reported to produce lignin-rich residues, compared to non-Bt (NBt) corn, suggesting it is more resistant to decomposition. As the Bt gene is expressed selectively in stem and leaf tissue, it could affect lignin distribution in corn, which naturally has greater lignin content in roots than in stems and leaves. Our objective was to evaluate the effects of corn plant components, the Bt gene and elevated-lignin inputs on decomposition. Roots, stems and leaves from Bt corn and NBt corn isolines enriched with ¹³C and ¹⁵N were finely ground and mixed separately with soil, then incubated at 20 °C for 36 weeks. The effect of elevated lignin on decomposition was tested by adding a commercial lignin source (indulin lignin) to half of the samples. In addition to weekly CO₂ analysis and regular measurement of N mineralization, the degree of lignin degradation was evaluated at 1 and 36 weeks from the acid to aldehyde ratio (Ad/Al) of vanillyl and syringyl lignin-derived phenols. The CO₂ production and N mineralization was lower in root-amended soils than stem- and leaf-amended soils. The Bt genetic modification increased CO₂ production from stem-amended soils (P < 0.05) and decreased N mineralization in root-amended soils. The ¹³C and ¹⁵N results also showed more residue-C and -N retained in soils mixed with NBt stem residues. After 36 weeks leaf- and stem-amended soils with indulin lignin had a lower Ad/Al ratio and were less degraded than soils without exogenous lignin. In conclusion, plant lignin and nitrogen contents were good predictors of CO₂ production and N mineralization potential. Corn roots decomposed more slowly than aboveground components emphasizing the importance of recalcitrant root residues in sustaining the organic matter content of soil.     

Phytotoxizität von Thallium (Tl) in Hydrokultur Teil 1: Einfluß von Tl(I) auf das Wachstum und die Schwermetallgehalte von Erbsen- und Ackerbohnenpflanzen

Phytotoxicity of Thallium (Tl) in Culture Solution Part 1: Effects of Tl(I) on the Growth and Heavy Metal Contents of Pea and Field Bean Plants The effects of TlNO₃ and Tl(I)EDTA on growth and heavy metal contents of pea plants (Pisum sativum L. cv. Aromata) and field bean plants (Vicia faba L. cv. Hangdown) were compared in hydroponic culture experiments. In the presence of TlNO₃, the essential heavy metals were available to the plants in their ionic forms. When Tl(I)EDTA was present the essential heavy metals were available as chelated complexes. TIN03 content of each organ was increased. The highest TI content was found within the stems. The increased TI contents were accompanied by depressed Mn, Zn, and Cu contents of the roots and depressed Mn contents of the stems, but increased Fe contents of the stems. Substitution of TIN03 by TI(1)EDTA resulted in a stronger growth inhibition of the pea plants, and higher TI contents of each organ. The highest TI content was found within the stems. TI(1)EDTA depressed Mn in the roots, but increased Fe and Mn in the stems, and Fe, Zn and Cu in the leaves. The increases may due to concentration by growth inhibition. The growth of the field bean was not effected by TIN03 nor by TI(1)EDTA. The field bean contained most of the TI within the roots and translocated only relatively small amounts to the shoots. This pattern was independent of the TI compound. Increasing concentrations of TIN03 resulted in depressed Mn and Zn contents of the roots, and Mn contents of the stems. Chelation of Tl(1) resulted in a decrease of the TI content of each organ. TI(1)EDTA depressed only the Mn content of the roots.     

Mineralisation of C and N from root, stem and leaf residues in soil and role of their biochemical quality

The influence of biochemical characteristics of 15 crop residues on C and N mineralisation in soil was investigated by following the decomposition of roots, stems and leaves of four subtropical species and one temperate species buried into the soil. The C, N and polyphenols contents were measured in different biochemical pools obtained from residues of the different organs. The mineralisation of root C was significantly lower than that of leaves and stems. Chemical analysis showed a higher polyphenol content in the leaves and a higher ligninlike content in the roots. Carbon and N mineralisation were simulated with the STICS decomposition submodel and tested against the data set. The model predicted leaf and stem C mineralisation for all five species fairly accurately, but failed to predict root C mineralisation, indirectly revealing the more complex composition of the root tissue. The results showed the interest of separately considering the different plant parts when studying plant residue decomposition and the need to develop other methods of residue quality characterisation to improve the prediction of residue decomposition.     

Ammoniakemissionen aus alternden Pflanzen und bei der Zersetzung von Ernterückständen

Ammonia emissions from senescing plants and during decomposition of crop residues NH₃ emissions from plant stands, measured under simulated environmental conditions with the wind tunnel method, ranged between 0.8 and 1.4% of the N content of the shoot, equivalent to 1.1 to 2.9 kg NH₃-N ha^?1. The highest emissions were observed in faba beans whereas the emissions in winter wheat, spring rape and white mustard were lower. The total NH₃ emissions were not affected by removing a part of the ears (sink reduction), but emissions occurred earlier, as did the plant senescence. This suggests that the NH₃ emissions are closely related to senescence. NH₃ emissions from decomposing crop residues ranged from 0.9 to 3.7% of the N content. The emissions from sugar beet leaves and potato shoots with high water content reached from 8.6 up to 12.6 kg N ha^?1, whereas the emissions from field bean straw with high dry matter and N content were relatively low. (3.1 kg N ha^?1, or 0.9% of the N content). The NH₃ emissions from sugar beet leaves were reduced by 81% by ploughing and 63% by mulching.     

Turnover of grain legume N rhizodeposits and effect of rhizodeposition on the turnover of crop residues

The turnover of N derived from rhizodeposition of faba bean (Vicia faba L.), pea (Pisum sativum L.) and white lupin (Lupinus albus L.) and the effects of the rhizodeposition on the subsequent C and N turnover of its crop residues were investigated in an incubation experiment (168 days, 15 °C). A sandy loam soil for the experiment was either stored at 6 °C or planted with the respective grain legume in pots. Legumes were in situ ¹⁵N stem labelled during growth and visible roots were removed at maturity. The remaining plant-derived N in soil was defined as N rhizodeposition. In the experiment the turnover of C and N was compared in soils with and without previous growth of three legumes and with and without incorporation of crop residues. After 168 days, 21% (lupin), 26% (faba bean) and 27% (pea) of rhizodeposition N was mineralised in the treatments without crop residues. A smaller amount of 15–17% was present as microbial biomass and between 30 and 55% of mineralised rhizodeposition N was present as microbial residue pool, which consists of microbial exoenzymes, mucous substances and dead microbial biomass. The effect of rhizodeposition on the C and N turnover of crop residues was inconsistent. Rhizodeposition increased the crop residue C mineralisation only in the lupin treatment; a similar pattern was found for microbial C, whereas the microbial N was increased by rhizodeposition in all treatments. The recovery of residual ¹⁵N in the microbial and mineral N pool was similar between the treatments containing only labelled crop residues and labelled crop residues + labelled rhizodeposits. This indicates a similar decomposability of both rhizodeposition N and crop residue N and may be attributable to an immobilisation of both N sources (rhizodeposits and crop residues) as microbial residues and a subsequent remineralisation mainly from this pool.Abbreviations C or N_dec C or N decomposed from residues - C or N_mic microbial C or N - C or N_micres microbial residue C or N - C or N_min mineralised C or N - C or N_input added C or N as crop residues and/or rhizodeposits - dfr derived from residues - dfR derived from rhizodeposition - Ndfr N derived from residues - NdfR N derived from rhizodeposition - N_loss losses of N derived from residues - SOM soil organic matter - WHC water holding capacity     

Estimating N rhizodeposition of grain legumes using a N in situ stem labelling method

Grain legumes in crop rotations cause significant increases in yield for succeeding non-legumes, which cannot be explained simply by the small effect that legumes have on the soil nitrogen balance, as found in the analysis of N in crop residues. Besides known positive non-N-effects, other effects, mainly rhizodeposition and its contribution to the N balance and nitrogen dynamics after harvesting the grain, are poorly understood. In this study, N rhizodeposition, defined as root-derived N in the soil after removal of visible roots, was measured in faba bean (Vicia faba L.), pea (Pisum sativum L.) and white lupin (Lupinus albus L.). In a pot experiment the legumes were pulse labelled in situ with ¹⁵N urea using a cotton wick method. About 84% of the applied ¹⁵N was recovered for the three legume species at maturity. The ¹⁵N was comparatively uniformly distributed among plant parts. The N rhizodeposition constituted 13% of total plant N for faba bean and pea and 16% for white lupin at maturity, about 80% of below ground plant N, respectively. Some 7% (lupin)-31% (pea) of the total N rhizodeposits were recovered as micro-roots by wet sieving (200 μm) the soil after all visible roots had been removed. Only 14-18% of the rhizodeposition N was found in the microbial biomass and a very small amount of 3-7% was found in the mineral N fraction. In pea, 48% and in lupin 72% of N rhizodeposits could not be recovered in the mentioned pools and a major part of the unrecovered N was probably immobilised in microbial residues. The results of this study clearly indicate that N rhizodeposition from grain legumes represent a significant pool for N balance and N dynamics in crop rotations.     

Characteristics,Residue Decomposition,and Carbon Mineralization of Leguminous and Spontaneous Plants in Coffee Systems

We investigated the chemical and biochemical composition, residue decomposition, and mineralization rate of leguminous (Cajanus cajan, Crotalaria spectabilis, and Lablab purpureus) and spontaneous vegetation in two experimental coffee systems in southeast Brazil. The nitrogen (N) content of the shoot biomass varied from 19.3 to 45.7 g kg^?1, and phosphorus (P) content ranged from 1.6 to 3.8 g kg^?1. C. cajan contained the greatest values of N and P, whereas spontaneous plants had the lowest values. In both areas, spontaneous vegetation had the greatest values of carbon (C) / P, C/N, polyphenol/N, and (lignin + polyphenol) / N ratios. Decomposition rate increased in the order C. cajan < C. spectabilis < L. purpureus < spontaneous vegetation. There was no correlation between the chemical and biochemical composition and the decomposition rate under field conditions. However, the cumulative carbon dioxide (C-CO₂) produced by the residues under laboratory conditions was correlated positively with initial contents of N and P and negatively with polyphenol/N and (lignin + polyphenol) / N ratio (P < 0.01) throughout the sampling period. The low nutrient content, especially for N, of spontaneous vegetation is compensated by the greater decomposition rate under natural conditions than that of introduced species. Management of the spontaneous plants is therefore an attractive alternative for sustainable agriculture.     

Carbon mineralization of tree leaf litter and crop residues from poplar-based agroforestry systems in Northeast China: A laboratory study

Tree leaf litter and crop residues (fine roots and straw) of the two main crops (maize and peanut) collected from temperate poplar-based agroforestry systems in Liaoning Province, China, were used in a laboratory decomposition experiment. The objectives were to assess the decomposition dynamics of individual plant residues of varying quality and to examine whether interactive effects between poplar litter and crop residues exist during decomposition. Rates of residue decomposition were measured as CO₂ production. Peanut roots decomposed faster than the other individual residues due to their high N and P concentrations and low C/N ratio. There were additive effects between poplar litter and crop residues during decomposition, even though significant differences existed in the initial nutrient concentrations of residues. Our results suggest that legume crops can produce high quality residues and thus have the potential to promote nutrient cycling. Therefore, legume crops have an advantage over other crops for intercropping in temperate agroforestry systems from the viewpoint of sustaining soil fertility.     

Nitrogen acquisition by pea and barley and the effect of their crop residues on available nitrogen for subsequent crops

Nitrogen acquisition by field pea (Pisum sativum L.) and spring barley (Hordeum vulgare L.) grown on a sandy loam soil and availability of N in three subsequent sequences of a cropping system were studied in an outdoor pot experiment. The effect of crop residues on the N availability was evaluated using ¹⁵N-labelled residues. Field pea fixed 75% of its N requirement and the N₂ fixation almost balanced the N removed with the seeds. The barley crop recovered 80% of the ¹⁵N-labelled fertilizer N supplied and the N in the barley grain corresponded to 80% of the fertilizer N taken up by the crop. The uptake of soil-derived N by a test crop (N catch crop) of white mustard (Sinapis alba L.) grown in the autumn was higher after pea than after barley. The N uptake in the test crop was reduced by 27% and 34% after pea and barley residue incorporation, respectively, probably due to N immobilization. The dry matter production and total N uptake of a spring barley crop following pea or barley, with a period of unplanted soil in the autumn/winter, were significantly higher after pea than after barley. The barley crop following pea and barley recovered 11% of the pea and 8% of the barley residue N. The pea and barley residue N recovered constituted only 2.5% and <1%, respectively, of total N in the N-fertilized barley. The total N uptake in a test crop of mustard grown in the second autumn following pea and barley cultivation was not significantly influenced by pre-precrop and residue treatment. In the short term, the incorporation of crop residues was not important in terms of contributing N to the subsequent crop compared to soil and fertilizer N sources, but residues improved the conservation of soil N in the autumn. In the long-term, crop residues are an important factor in maintaining soil fertility and supplying plant-available N via mineralization.     

Carbon costs of nitrate reduction in broad bean (Vicia faba L.) and pea (Pisum sativum L.) plants

The present study aimed at the assessment of carbon (C) costs for nitrate reduction by measuring the additional CO₂ amounts released from roots of nitrate‐fed plants in comparison with urea‐fed plants. Only roots were suitable for these determinations, because nitrate reduction in illuminated shoots is fed nearly exclusively by reducing equivalents coming directly from photosynthetic processes. Therefore, in a first experiment, the sites of nitrate reduction were determined in nodule‐free broad bean (Vicia faba L.) and pea (Pisum sativum L.) plants grown in pots filled with quartz sand and supplied with KNO₃. The extent of nitrate reduction in the various plant organs was determined by measuring in vitro nitrate reductase activity and in situ ¹⁵NO reduction. Only between 9% and 16% of nitrate were reduced in roots of German pea cultivars, whilst 52% to 65% were reduced in broad bean roots. Therefore, C costs of the process could be determined only in broad bean, using an additional pot experiment. The C costs amounted to about 4.76 mol C (mol N)^–1 or 4 mg C (mg N)^–1, similar to those measured earlier for N₂ fixation. The high proportion of nitrate reduction in shoots of pea plants implies that only very little C is required for this nitrate fraction. This can explain the better root growth of nitrate‐nourished pea plants in comparison with N₂‐fixing organisms, which need C compounds for N₂ reduction in roots. Moreover, a different availability of photosynthates in roots of plant genotypes could explain physiologically the occurrence of “shoot and root reducers” in nature.     

Leaching and plant offtake of N in field pea/cereal cropping sequences with incorporation of 15N-labelled pea harvest residues

Abstract. Field peas (Pisum sativum L.) were grown in sequence with winter wheat (Triticum aestivum L.) or spring barley (Hordeum vulgare L.) in large outdoor lysimeters. The pea crop was harvested either in a green immature state or at physiological maturity and residues returned to the lysimeters after pea harvest. After harvest of the pea crop in 1993, pea crop residues (pods and straw) were replaced with corresponding amounts of ¹⁵N‐labelled pea residues grown in an adjacent field plot. Reference lysimeters grew sequences of cereals (spring barley/spring barley and spring barley/winter wheat) with the straw removed. Leaching and crop offtake of ¹⁵N and total N were measured for the following two years. These treatments were tested on two soils: a coarse sand and a sandy loam. Nitrate concentrations were greatest in percolate from lysimeters with immature peas. Peas harvested at maturity also raised the nitrate concentrations above those recorded for continuous cereal growing. The cumulative nitrate loss was 9–12 g NO₃‐N m^–2 after immature peas and 5–7 g NO₃‐N m^–2 after mature peas. Autumn sown winter wheat did not significantly reduce leaching losses after field peas compared with spring sown barley. ¹⁵N derived from above‐ground pea residues accounted for 18–25% of the total nitrate leaching losses after immature peas and 12–17% after mature peas. When compared with leaching losses from the cereals, the extra leaching loss of N from roots and rhizodeposits of mature peas were estimated to be similar to losses of ¹⁵N from the above‐ground pea residues. Only winter wheat yield on the coarse sand was increased by a previous crop of peas compared to wheat following barley. Differences between barley grown after peas and after barley were not statistically significant. ¹⁵N lost by leaching in the first winter after incorporation accounted for 11–19% of ¹⁵N applied in immature pea residues and 10–15% of ¹⁵N in mature residues. Another 2–5% were lost in the second winter. The ¹⁵N recovery in the two crops succeeding the peas was 3–6% in the first crop and 1–3% in the second crop. The winter wheat did not significantly improve the utilization of ¹⁵N from the pea residues compared with spring barley.     

长期不同施氮处理玉米根茬的田间分解特性

以7年氮肥定位试验地玉米根茬为研究对象,通过把玉米根茬按2%比例与15 cm和45 cm土层深度的土壤混合后田间埋袋的方法,研究长期不同施氮量处理[分别为0 kg(N)?hm?2、120 kg(N)?hm?2和240 kg(N)?hm?2]的玉米根茬(分别用R0、R120、R240表示),在陕西省长武黑垆土中埋藏分解1 a后对土壤碳、氮组分的影响及根茬有机碳的分解特性。与未添加玉米根茬的对照土壤相比,玉米根茬加入能够显著增加各层土壤的微生物量碳、可溶性有机碳和矿质态氮含量,3种施氮量处理间差异不显著。随着分解时间延长,土壤可溶性有机物中结构相对复杂的芳香类化合物比例逐渐增加。分解1 a后,R0、R120和R240根茬的有机碳残留率在15 cm土层中分别为44.4%、35.3%和34.9%,在45 cm土层中分别为53.3%、44.3%和42.5%。R0根茬的碳残留率显著高于R120和R240;玉米根茬在15 cm土层的碳分解率和分解速率常数显著高于45 cm土层。采用一级动力学方程拟合玉米根茬碳残留率变化结果显示,R0、R120和R240根茬有机碳分解95%所需要的时间在45 cm土层比15cm土层分别长3.2 a、2.3 a和1.9 a。氮肥施用量影响玉米根茬在土壤中的分解特性,在评价农田氮肥施用与土壤固碳时,应考虑不同氮肥用量下残茬养分组成及其在土壤中分解的差异。     

影响菜豆体内铁再利用效率的因素及其机理

本文在人工气候室中，用营养液培养方法，并结合同位素示踪技术研究了铁的供应状况，两种形态氮素（ＮＯ＾－３－Ｎ和ＮＨ＾＋４－Ｎ）及叶处遮光对菜豆体内铁再利用效率的影响，并对其有关机理进行了深入的研究。结果表明，铁的缺乏有利于累积在根和初生叶中的铁身新生组织中转移，铁的再利用效率明显提高。无论有缺铁还供铁条件下，ＮＨ＾＋４－Ｎ的供应使得菜豆新叶中活性铁含量、新叶叶绿素含量及体内铁的再利用效率都明显高于Ｎ     

Non-additive effects vary with the number of component residues and their mixing proportions during residue mixture decomposition: A microcosm study

Poplar leaf litter and crop residues (leaves and stems) of two main crops (soybean and maize) collected from semiarid agroforestry systems of Northeast China were used in our microcosm study. The aims were to examine whether non-additive effects (synergistic or antagonistic) between poplar leaf litter and crop residues exist during decomposition and to identify the influence of residue mixing proportion on the incidence of non-additive effects of residue mixture for the same plant residues. We determined residue decomposition rate by measuring mass loss and N release. Synergistic effects between poplar leaf litter and crop residues were more common than additive effects in terms of mass loss and N release. Moreover, the interactive effects between tree leaf litter and crop residues on decomposition varied with the number of component residues and their mixing proportion. Three-residue mixtures produced synergistic effects on mass loss and N release, although two-residue mixtures showed an additive effect in some cases. In addition, as compared with equal proportion, mixing residues with unequal proportion increased the incidence of non-additive effects during decomposition of residue mixture. These findings highlight that residue decomposition dynamics in ecosystems should be assessed on the basis of plant residue mixtures and their mixing proportions, which may help us better understand nutrient dynamics and guide our decisions on nutrient management.     

Peanut residues supply minimal plant-available nitrogen on a major soil series in the USA peanut basin

Field observations have shown that a substantial portion of peanut leaves abscise in windrows during pod curing, leading to an uneven distribution of leaves and stems when intact residues are spread during harvest. Possible differences in nitrogen (N) mineralization rates between peanut leaf and stem residues may lead to spatial and temporal variability in available N during subsequent crops. The objective of this study was to quantify N mineralization in soil amended with different peanut residue components under simulated conventional and conservation tillage practices. A 252-day microlysimeter incubation was conducted in which peanut leaves, stems and a 1:1 mixture of leaves:stems from three varieties were incorporated or placed on the soil surface to simulate conventional or conservation tillage, respectively. Soils were periodically leached to assess N mineralization compared with a soil-only control. Nitrogen mineralization was only affected by residue component. Averaged over variety and residue placement, soil amended with leaves mineralized 10% more N relative to the control or soil containing stems. It was estimated that leaves supplied 25 kg N ha⁻¹ over 252 days at 0–15 cm soil depth, which would likely be insufficient to induce a yield response by a subsequent crop. This study suggests that uneven distribution of peanut leaf and stem residues following harvest causes only minor spatial and temporal variability in available N during subsequent crop growth. These results support the growing body of evidence indicating that peanut residue N contributions to subsequent crops are negligible in the peanut basin of the south-eastern USA.     

Decomposition of barley straw in a subarctic soil in the field

Summary The mass loss and N dynamics of barley stems and leaves, placed on the soil surface or buried, were examined over two summers. There was little difference in mass loss or N dynamics in straw placed 7.5 or 15 cm deep. However, the surface straw lost mass much more slowly and immobilized more N for a longer time than the buried straw. Filter paper had a slow rate of mass loss initially, but once started, lost mass much more rapidly than either the barley stems or leaves. Loss of mass was closely correlated with the cellulose loss in straw, whether buried or placed on the soil surface. The sustained rate of mass loss was 6.3 and 7.0% month^-1, respectively, for surface and incorporated leaves compared with 3.5 and 4.3% month^-1, for surface and incorporated stems. The greater loss sustained by the leaves was attributed to a lower lignin content rather than a higher N content, because the addition of N to the straw after 30 days in the field failed to increase CO₂ evolution. Maximum net N immobilization occurred within 30 days for all the barley straw, except for the stems placed on the ground surface, which did not reach maximum N immobilization until the second summer. Immobilization and mineralization of N were estimated for a 3000 kg ha^-1 grain crop. Surface straw immobilized 3.8 kg N ha^-1 in the 1st year and 9 kg N ha^-1 in the 2nd year, whereas incorporated straw immobilixed 3.5 kg N hs^-1 in the 1st year and mineralized 4.5 kg N ha^-1 in the 2nd year. Thus, in Alaska, residue management does not affect N fertilizer requirements in the 1st year, but an additional 13.5 kg N ha^-1 is required for surface residues in the 2nd year.     

Lignin is involved in the reduction of Verticillium dahliae var. longisporum inoculum in soil by crop residue incorporation

Verticillium wilt is an increasing problem in European cauliflower production. In this study, several crop residues were screened for their ability to reduce the viability of microsclerotia when incorporated into soil. In addition, the role of fungitoxic volatiles and lignin in the crop residue-mediated reduction in microsclerotia viability was studied.Broccoli (Brassica oleracea var. italica), cauliflower (B. oleracea var. botrytis), Indian mustard (Brassica juncea), ryegrass (Lolium perenne) and corn (Zea mays) were incorporated in naturally infested soil samples collected from two cauliflower fields in Belgium, labelled Is1 and S3. The effectiveness in reducing the viability of microsclerotia depended on the soil sample and on the type of residue. In the Is1 soil, broccoli, cauliflower and ryegrass incorporation significantly reduced the inoculum level by more than 90%, while Indian mustard significantly reduced numbers of viable microsclerotia by 50%. In the S3 soil, broccoli, cauliflower and Indian mustard were not effective, whereas ryegrass and corn incorporation reduced the microsclerotia level by 50% or more. In conclusion, incorporation of ryegrass and corn was more effective than incorporation of crucifer residues.In the conditions tested, fungicidal volatile compounds did not play an important role in Verticillium microsclerotia reduction in soil. Volatiles from broccoli and cauliflower did not affect microsclerotia viability in an in vitro bioassay, whereas the volatiles from Indian mustard killed the microsclerotia. Indian mustard incorporation in soil, however, only had a minor effect on microsclerotia viability.In the S3 soil, 1% (w/w) Kraft pine lignin, a waste product of the paper industry, had to be added to observe a significant reduction on the viability of microsclerotia, whereas in the Is1 soil, a significant effect was observed when 0.1% (w/w) Kraft pine lignin was added. Acid-insoluble lignin was extracted from all crop residues previously tested. Crop residues with high lignin content seemed to be more effective than crop residues with low lignin content. The reduction of Verticillium microsclerotia viability depended on lignin type and on crop structure, since lignin extracted from cauliflower leaves was more effective than lignin extracted from cauliflower stems and corn leaves were more effective than corn roots. Microsclerotia reduction was higher after fresh residue incorporation than after incorporation of their extracted acid-insoluble lignin, indicating that the effect of crop residue incorporation on microsclerotia viability cannot be explained solely by the effects of lignin.Incorporation of lignin-rich substrates in soil may open up new perspectives for integrated control of Verticillium.     

Decomposition of 15N-labelled catch-crop residues in soil: evaluation of N mineralization and plant-N uptake potentials under controlled conditions

The decomposition of ¹⁵N-labelled catch-crop materials (rape, radish and rye), obtained from field experiments, was studied in a chalky Champagne soil during a 60-week incubation at 28°C. Mineralized N was assumed to come from either labile or recalcitrant fractions of plant residues. The labile fraction represented about one-third of the catch-crop N; its mineralization rate constant varied from 0.06 to 0.12 d^?1. The decomposition rate of the recalcitrant N fraction ranged from 0.03 × 10^?2 to 0.06 × 10^?2 d^?1. Catch-crop species and rate of incorporation had no effect on N residue mineralized at the end of incubation. The decomposition of labelled rye was monitored in the same soil during a 5-month pot experiment to determine the N availability to an Italian ryegrass crop and the effect of plants on the decomposition processes. The ¹⁵N-rye decomposed rapidly both in the presence or absence of Italian ryegrass, but the amounts of N mineralized were influenced by the presence of living roots: 42% of the ¹⁵N in labelled rye was present as inorganic N in the pots without plants after 5 months, compared with only 32% in the ryegrass crop. Comparison of microbial-biomass dynamics in both treatments suggested that there had been preferential utilization by soil micro-organisms of materials released from the living roots than the labelled plant residues.     

Leaf litter decomposition in an upper montane rainforest in Sri Lanka

In a field study in an upper mountain rain forest in Sri Lanka leaf litter decay rates for nine tree species were measured using the standard litterbag method. The leaf species showed a wide variation in decomposition rates with k values ranging from 0.19 to 9.6 (t_0.99 values ranging from 0.5 to 24 years), but it was possible to recognize fast, medium and slow decomposition groups. While there were considerable differences in physical and chemical litter properties these were poor predictors of decomposition rates. There was considerable variation in the N, P and lignin contents of mature green leaves and freshly fallen dead leaves of the different tree species. Percent resorption of N varied from 0 (one species) to 56 and of P from 0 (three species) to 73. There were no consistent patterns of nutrient mobilization and net release of N and P in the five leaf litter species studied.