Effect of liming on EUF-nutrient fractions in the soil,on nutrient contents of grape leaves and on grape yield

Summary In pot experiments with vine, liming significantly raised EUF-Ca 20°C as well as EUF-Ca 80°C values of an acid clay soil (pH 4.2). This resulted in a marked rise in Ca contents of vine leaves (Table 2). High amounts of K fertilizers without lime raised mainly the EUF-Ca 20°C values whereas the EUF-80°C values remained at a low level (Table 3). Liming lowered the EUF-K 20°C values and as a result the ratio EUF-K 80°C C/EUF-K 20°C increased from 0.7 to 1.0.High K applications raised the K content of the leaves at flowering stage but at grape ripening a marked decrease in K content was observed (Table 5). In contrast, the application of both lime and K fertilizer raised the K content of leaves at both flowering and ripening. Grape yield increased as well (Table 11).Liming raised the EUF-P values of the soil and to a lesser extent the P contents of leaves (Tables 6 and 7).High K applications without lime raised the Mn contents of leaves (Table 9), Exchange processes due to K fertilizer addition were reflected in increased EUF-Mn values (Table 9).The highest yield (three-year average) was obtained in a high K treatment (22 g K₂O/pot) in combination with lime (40 g CaO/pot).     

EUF-analysis of tea soils of Southern India and tea productivity

Summary The relationship between EUF extractable nutrients and conventional soil test extractable nutrients in the acid soils of Southern India on one hand and that between EUF values and tea productivity on the other are described. Close correlation exists between EUF-NO₃–N at 20°C and CuSO₄–Ag₂SO₄-extractable NO₃–N (r=0.98^***), EUF-N_org and Morgan's reagent extractable NH₄–N (r=0.97^***), total EUF-N and CuSO₄–Ag₂SO₄-extractable NO₃–N plus Morgan's reagent NH₄–N (r=0.96^***), EUF-P at 20°C and modified Bray II-P (r=0.93^***) and EUF-P at 20°C plus that at 80°C and modified Bray II-P (r=0.91^***). The EUF-K at 20°C shows close correlation with NH₄OAc–K (r=0.80^***), Ag-thiourea-K (r=0.86^***) and Morgan's reagent-K (r=0.84^***) whereas the EUF-K at 80°C shows close correlation with the difference in K contents of NH₄OAc–K and Ag-thiourea-K (r=0.92^***) or of NH₄OAc–K and Morgan's reagent-K (r=0.93^***) and fixed NH₄–N (r=0.89^***). EUF-Ca, EUF-Mg and EUF-Mn do not show any relationship with conventional soil test values. Tea productivity is strongly associated with EUF-N and EUF-P extracted at 20°C.     

Spatial and Temporal Variation of Roots, Arbuscular Mycorrhizal Fungi, and Plant and Soil Nutrients in a Mature Pinot Noir (Vitis vinifera L.) Vineyard in Oregon, USA

Soil and crop management practices may influence biomass growth and yields of cotton (Gossypium hirsutum L.) and sorghum (Sorghum bicolorL.) and sequester significant amount of atmospheric CO₂in plant biomass and underlying soil, thereby helping to mitigate the undesirable effects of global warming. This study examined the effects of three tillage practices [no-till (NT), strip till (ST), and chisel till (CT)], four cover crops [legume (hairy vetch) (Vicia villosa roth), nonlegume (rye) (Secale cerealeL), hairy vetch/rye mixture, and winter weeds orno covercrop], and three N fertilization rates (0, 60–65, and 120–130 kg N ha ^–1) on the amount of C sequestered in cotton lint (lint + seed), sorghum grain, their stalks (stems + leaves) and roots, and underlying soil from 2000 to 2002 in central Georgia, USA. A field experiment was conducted on a Dothan sandy loam (fine-loamy, kaolinitic, thermic, Plinthic Kandiudults). In 2000, C accumulation in cotton lint was greater in NT with rye or vetch/rye mixture but in stalks, it was greater in ST with vetch or vetch/rye mixture than in CT with or without cover crops. Similarly, C accumulation in lint was greater in NT with 60 kg N ha ^–1 but in stalks, it was greater in ST with 60 and 120 kg N ha ^–1 than in CT with 0 kg N ha ^–1. In 2001, C accumulation in sorghum grains and stalks was greater in vetch and vetch/rye mixture with or without N rate than in rye without N rate. In 2002, C accumulation in cotton lint was greater in CT with or without N rate but in stalks, it was greater in ST with 60 and 120 kg N ha ^–1 than in NT with or without N rate. Total C accumulation in the above- and belowground biomass in cotton ranged from 1.7 to 5.6 Mg ha ^–1 and in sorghum ranged from 3.4 to 7.2 Mg ha ^–1. Carbon accumulation in cotton and sorghum roots ranged from 1 to 14% of the total C accumulation in above- and belowground biomass. In NT, soil organic C at 0–10 cm depth was greater in vetch with 0 kg N ha ^–1 or in vetch/rye with 120–130 kg N ha ^–1 than in weeds with 0 and 60 kg N ha ^–1 but at 10–30 cm, it was greater in rye with 120–130 kg N ha ^–1 than in weeds with or without rate. In ST, soil organic C at 0–10 cm was greater in rye with 120–130 kg N ha ^–1 than in rye, vetch, vetch/rye and weeds with 0 and 60 kg N ha ^–1. Soil organic C at 0–10 and 10–30 cm was also greater in NT and ST than in CT. Since 5 to 24% of C accumulation in lint and grain were harvested, C sequestered in cotton and sorghum stalks and roots can be significant in the terrestrial ecosystem and can significantly increase C storage in the soil if these residues are left after lint or grain harvest, thereby helping to mitigate the effects of global warming. Conservation tillage, such as ST, with hairy vetch/rye mixture cover crops and 60–65 kg N ha ^–1 can sustain C accumulation in cotton lint and sorghum grain and increase C storage in the surface soil due to increased C input from crop residues and their reduced incorporation into the soil compared with conventional tillage, such as CT, with no cover crop and N fertilization, thereby maintaining crop yields, improving soil quality, and reducing erosion.     

Application of the EUF procedure in sugar beet cultivation

Summary The relationship between the EUF-nutrient fractions in the soil on the one hand and the nutrient uptake of sugar beet as well as root yield and quality (polarization, α-amino N etc.) on the other is described on the basis of results obtained over several years in surveys conducted in farmers' fields (5000–6000 fields under sugar beet per year) and in field experiments (25–35 sites per year). Statistically significant close correlations with the respective parameters were found for the following EUF nutrient fractions: EUF-NO₃, EUF-P, EUF-K, EUF-Na, EUF-B and EUF-Mn. Within five years it was possible to determine the EUF-nutrient values which are required for the production of 9 t sugar/ha. These EUF values are the following: Ca: 65–70 mg/100 g at 20°C K: 11–15 mg/100 g at 20°C (depending on the clay content) Mg: 3–5 mg/100 g at 20°C Na: 2–3 mg/100 g at 20°C P: 1.4–1.6 mg/100 g at 20°C For calculation of the N fertilizer requirements of sugar beet it is suggested to use the sum of the EUF-extractable N amounts. It was found in Austria, Yugoslavia and Denmark over a period of 3 years that the EUF-N value of 1 mg/100 g soil determined between June and September was equivalent to 40 kg N/ha. If, for example, the analysed soil contains 3 mg EUF-N/100 g, 3×40=120 kg N/ha will be available to the sugar beet crop in the following year.     

Soybean yield response to residual NO3−N and applied N

Summary During 1976 through 1978, 10N treatments (combinations of N application times and rates) were used in a corn study. Those treatments created different levels of soil NO ₃ ^– –N content that were well-suited to a study of the influence of residual NO ₃ ^– –N and applied N on soybean yield. In April 1979 we applied ammonium nitrate at rates of 0, 75, or 150 kg N/ha to three subplots formed from each of the whole plots (previous N treatment plots). With N fertilization in 1979, seed yield increased where the residual NO ₃ ^– –N amount was less than 190 kg/ha but decreased where the residual amount was greater than 190 kg/ha. As the NO ₃ ^– –N content in the soil increased by 1 kg/ha, the soybean yield increase due to N fertilization in 1979 decreased by approximately 4 kg/ha.Contribution no. 82-368-J, Dep. of Agronomy, Kansas Agric. Exp. Stn., Manhattan, KS 66506, USA     

Influence of slurry applications on the EUF-N fractions in the soil

Summary Increasing quantities of slurry (30, 60 and 90 m³/ha as well as 60 m³/ha + DIDIN) were applied to two sandy soils both in September and in December 1982. During the 1982/83 winter EUF-N was determined in soil horizons (0–30 cm, 30–60 and 60–90 cm).EUF-NO₃ and EUF-N_org clearly reflected the different quantities of slurry applied. The retarding effect of DIDIN on nitrification could also be demonstrated by means of the EUF-N contents.Due to the mild and humid climate prevailing in the winter of 1982/83 slurry-NO₃ of the September applications had obviously been leached out of the 0–60 cm soil layer in all treatments by February and even out of the 60–90 cm layer by March 24. Translocation of NO₃ was also observed for slurry applied in December. But in this case on March 24 the EUF-NO₃ contents in the 60–90 cm layer still reflected the quantities of slurry applied four months earlier.After slurry application the EUF-N_org fraction of a soil initially consists mainly of NH ₄ ⁺ which is rapidly oxidized to NO₃ and transferred in this form to deeper layers. As a consequence a rapid decline in EUF-N_org fraction is observed. It could therefore be expedient to consider the N_org and EUF-NH ₄ ⁺ fractions separately when slurry applications are concerned.     

Changes of EUF-N and EUF-K fractions in three deep grey-brown luvisols during 18 months under fallow

Summary The EUF-N and EUF-K contents of deep grey-brown luvisols under fallow were investigated over a period of 18 months.EUF-NO₃-N increased continuously during the spring and summer of 1983, reaching their peak in September/October. They declined in the winter of 1984, and increased again during the spring and summer of the same year.During the spring and winter EUF-N_org was higher than EUF-NO₃-N. A decline in EUF-N_org due to mineralization was associated with an increase of EUF-NO₃-N. EUF-N_org increased due to mobilization of soil N in April/May. EUF-N_org also increased in autumn 1983 as a consequence the incorporation of mineral nitrogen into this fraction. When mineral N was incorporated EUF-NO₃-N declined.EUF-N_org in the subsoil was lower than in the topsoil. EUF-NO₃-N in the subsoil decreased as EUF-N_org increased. It may therefore be assumed that the higher the content of EUF-N_org in the subsoil the more mineral nitrogen will be immobilized.     

Relative efficiency of N fertilizers as influenced by N-serve in the potato crop

Summary Field experiments, on potato, were conducted in the alluvial soils of Ludhiana, in 1976–77 and 1980–81, to investigate the relative efficiency of N fertilizers as influenced by a nitrification inhibitor (N-serve). In the absence of N-serve, sulphate of ammonia (S/A) and calcium ammonium nitrate (CAN) proved superior to urea, on an equal N basis, in almost all the yield characters and yield, but urea treated with N-serve tended to equal S/A and proved better than CAN. The inhibitor increased the N-uptake and N-recovery from urea and decreased the optimum basal dose of the fertilizer, by 10.8kg N/ha in 1976–77 and by 40.5 kg N/ha in 1980–81, without reducing the tuber yield in any of the two years. S/A and CAN did not profit from the treatment with N-serve.     

Relationship between EUF-K contents,K uptake and sugar yield of sugar beet in deep loess soils

Summary In field experiments with varying K fertilization (1981 and 1982) changes in EUF-K contents were studied in deep loess soils of Southern Lower Saxony under sugar beet. A significant positive linear relationship was found between EUF-K contents at 20°C and 200 V (15 mA) of the topsoils and quantities of K absorbed by sugar beet in both years. The corresponding regression lines for 1981 and 1982 are almost parallel, the only difference being the yield level which was higher in 1982.The relationship between EUF-K contents at 20°C of topsoils and sugar yields showed the same parallelism for the two years. Not much increase in sugar yield was found at EUF-K contents over 12 mg/100 g soil at EUF-K 80°C/EUF-K 20°C ratios between 0.5 and 0.7. To attain a sugar yield of 10 t/ha an EUF-K 20°C value of at least 12 mg/100 g soil is required for these deep soils at the beginning of the K uptake period. This finding confirms experiences gained over an 8-year period at the Tulln Sugar Factory (Austria) with fertilizer recommendations based on EUF.     

Soil nitrogen availability under grassland and cultivated corn

Summary Adjacent corn and ryegrass plots were fertilized with rates of 0, 50, 100, 150, and 200 kg N as ammonium nitrate/ha. Corn growing on this soil did not respond to fertilizer N while ryegrass responded to rates of up to 200 kg N/ha. The differences in N availability was also reflected in the higher profile NO₃–N under corn than under ryegrass. The same general trends occurred on a second soil, where N availability for the hay crop was also less than for corn crop. Compared with corn, hay responded more to N fertilizer and had lower soil NO₃–N levels.Grasslands appear to respond to higher N fertilizer rates than cultivated crops on the same soil.Vermont Agricultural Experiment Station Journal Article No. 495.     

Effects of D-D, Telone or dazomet applied to potato ridges in spring on potato cyst-nematode, Heterodera rostochiensis, in sandy loam and silt loam soils

Large amounts of dazomet (329, 439 kg/ha) applied to potato ridge soil in spring, before potatoes were planted, controlled potato cyst-nematode (Heterodera rostochiensis) in sandy loam and silt loam more effectively than large amounts of D-D (359, 448 kg/ha). In heavily infested sandy loam, 329 kg dazomet/ha or 857 kg methyl bromide/ha applied in spring 1969 or 439 kg dazomet/ha applied in autumn 1968, greatly decreased the number of larvae able to invade potato roots, so Majestic potatoes grew and yielded well without increasing the number of nematodes left in the soil after harvest. Large amounts of D-D or Telone applied to the topsoil in autumn or to the ridges in spring were less effective in controlling potato cyst-nematode or increasing potato yields. Applied in spring 1969 to silt loam ridges, 439 kg dazomet/ha had more effect than 448 kg D-D/ha on potato cyst-nematode and on the increase in yield of Majestic potato. The yield of Maris Piper potatoes (resistant to H. rostochiensis pathotype A) in infested silt loam was increased greatly by D-D, as much by 112 as by 224 or 448 kg/ha.     

Treating potato ridges in spring with aldicarb, D-D or dazomet to control potato cyst-nematode, Heterodera rostochiensis, in sandy clay and peat loam soils

Applied to potato ridge soil in spring, before potatoes were planted, small amounts of aldicarb (10-3 kg/ha or less) controlled potato cyst-nematodes (Heterodera rostochiensis Woll.) better than large amounts of dazomet (110–466 kg/ha) or D-D (102–439 kg/ha). Applied in spring 1968 and 1969 to heavily infested sandy clay soil 466 kg dazomet/ha allowed Majestic potatoes to grow and yield well in both years without increasing the number of nematodes in the soil after harvest, but in peaty loam dazomet was toxic to potato plants and, when applied in autumn, killed fewer nematodes. D-D in potato ridges in spring controlled nematodes less well than dazomet or aldicarb, but 896 kg D-D/ha injected in sandy clay soil in autumn increased potato yield the following year without increasing the number of nematodes after harvest.     

Response of wheat to levels of zinc and potash in calcareous soil

Summary A field experiment was conducted at Agricultural Research Institute, Dholi during Rabi 1976–77 in sandy loam soil to study the interaction between zinc and potash in wheat. Zinc and potash were applied to the soil in the form of ZnSO₄ and KCl respectively. Interaction between zinc and potash was found significant. Both the levels of zinc sulphate 12.5 kg/ha and 25 kg/ha being at par produced significantly higher grain yield over control. There was significant increase in grain yield with application of 40 kg and 80 K₂O/ha over control. Potash at the rate of 120 kg in combination with 25 kg Zinc sulphate/ha decreased the yield.     

Relationships between EUF-N fractions,N uptake and quality of sugar beet in deep loess soils of Southern Lower Saxony

Summary In field experiments conducted in 1981 on deep loess soils a significant correlation was obtained between EUF-N content in the topsoil and N in sugar beet roots as well as in whole plants. A very close correlation was found to exist between EUF-N values in June 1981 and -amino N in sugar beet roots at harvest. Also other quality criteria such as the contents of sugar, K and Na in roots and yield parameters correlated with EUF-N contents in topsoils.The inorganic and organic EUF-N fractions changed during the vegetation period due to both N uptake by the crop and mineralization. Therefore it appears to be expedient to use both fractions when calculating N fertilizer requirements.The correlation between EUF-N (topsoil samples drawn in the year preceding sugar beet) and sugar yield increases obtained by N fertilization that was found in Austria¹² was confirmed in our experiments with soils from Southern Lower Saxony.     

Nitrous oxide emissions following application of residues and fertiliser under zero and conventional tillage

Emissions of N₂O were measured following combined applications of inorganic N fertiliser and crop residues to a silt loam soil in S.E. England, UK. Effects of cultivation technique and residue application on N₂O emissions were examined over 2 years. N₂O emissions were increased in the presence of residues and were further increased where NH₄NO₃ fertiliser (200 kg N ha^–1) was applied. Large fluxes of N₂O were measured from the zero till treatments after residue and fertiliser application, with 2.5 kg N₂O-N ha^–1 measured over the first 23 days after application of fertiliser in combination with rye (Secale cereale) residues under zero tillage. CO₂ emissions were larger in the zero till than in the conventional till treatments. A significant tillage/residue interaction was found. Highest emissions were measured from the conventionally tilled bean (Vicia faba) (1.0 kg N₂O-N ha^–1 emitted over 65 days) and zero tilled rye (3.5 kg N₂O-N ha^–1 over 65 days) treatments. This was attributed to rapid release of N following incorporation of bean residues in the conventionally tilled treatments, and availability of readily degradable C from the rye in the presence of anaerobic conditions under the mulch in the zero tilled treatments. Measurement of ¹⁵N-N₂O emission following application of ¹⁵N-labelled fertiliser to microplots indicated that surface mulching of residues in zero till treatments resulted in a greater proportion of fertiliser N being lost as N₂O than with incorporation of residues. Combined applications of ¹⁵N fertiliser and bean residues resulted in higher or lower emissions, depending on cultivation technique, when compared with the sum of N₂O from single applications. Such interactions have important implications for mitigation of N₂O from agricultural soils.     

Methane and nitrous oxide exchange in differently fertilised grassland in southern Germany

We examined the effect of fertilisation (200 kg cattle slurry-N ha^–1 year^–1) on the exchange of N₂O and CH₄ in the soil–plant system of meadow agroecosystems in southern Germany. From 1996 to 1998, we regularly determined the gas fluxes (closed chamber method) and associated environmental parameters. N₂O and CH₄ fluxes were not significantly affected by fertilisation. N₂O fluxes at the unfertilised and fertilised plots were small, generally between 50 and –20 g N m^–2 h^–1. We identified some incidents of N₂O uptake. CH₄-C fluxes ranged from 1.3 to –0.2 mg m^–2 h^–1 and were not significantly different from 0 at both plots. We budgeted an annual net emission of 15.5 and 29.6 mg m^–2 N₂O-N and an annual CH₄-C net emission of 184.2 and 122.7 mg m^–2 at the unfertilised and fertilised plots, respectively. Apparently, rapid N mineralization and uptake in the densely rooted topsoil prevents N losses and the inhibition of CH₄ oxidation.     

Effects of planted tree fallows on soil nitrogen dynamics,above-ground and root biomass,N2-fixation and subsequent maize crop productivity in Kenya

The effects of planted fallows of Sesbania sesban (L.) Merr. and Calliandra calothyrsus (Meissner) on soil inorganic nitrogen dynamics and two subsequent maize crops were evaluated under field conditions in the highlands of eastern Kenya. Continuous unfertilised maize, maize/bean rotation and natural regrowth of vegetation (weed fallow) were used as control treatments. The proportion of symbiotic N₂-fixation was estimated by measuring both leaf ¹⁵N enrichment and whole-plant ¹⁵N enrichment by the ¹⁵N dilution technique for Sesbania and Calliandra, using Eucalyptus saligna (Sm.) and Grevillea robusta (A. Cunn) as reference species. Above- and below-ground biomass and N contents were examined in Sesbania, Calliandra, Eucalyptus and Grevillea 22 months after planting. Both the content of inorganic N in the topsoil and the quantity of N mineralised during rainy seasons were higher after the Sesbania fallows than after the other treatments. Compared to the continuous unfertilised maize treatment, both residual crop yields were significantly higher when mineral N (one application of 60 kg N ha^–1) was added. Furthermore, the second crop following the Sesbania fallow was significantly higher than the continuous maize crop. The above-ground biomass of the trees at final harvest were 31.5, 24.5, 32.5 and 43.5 Mg ha^–1 for the Sesbania, Calliandra, Grevillea and Eucalyptus, respectively. For the total below-ground biomass the values for these same tree species were 11.1, 15.5, 17.7, and 19.1 Mg ha^–1, respectively, of which coarse roots (>2 mm), including tap roots, amounted to 70–90%. About 70–90% of the N in Sesbania, and 50–70% in Calliandra, was derived from N₂-fixation. Estimates based on leaf ¹⁵N enrichment and whole-plant ¹⁵N enrichment were strongly correlated. The N added by N₂-fixation amounted to 280–360 kg N ha^–1 for Sesbania and 120–170 kg N ha^–1 for Calliandra, resulting in a positive N balance after two maize cropping seasons of 170–250 kg N ha^–1 and 90–140 kg N ha^–1, for Sesbania and Calliandra, respectively. All the other treatments gave negative N balances after two cropping seasons. We conclude that Sesbania sesban is a tree species well suited for short duration fallows due to its fast growth, high nutrient content, high litter quality and its ability to fix large amounts of N₂ from the atmosphere.     

Total denitrification and the ratio between N2O and N2 during the growth of spring barley

Summary Total denitrification (N₂O+N₂) and nitrous oxide emission were measured on intact soil cores using the acetylene inhibition technique.Total denitrification from the depth 0–8 cm during the growth period from April to August was 7 kg N/ha from plots supplied with 30 kg N/ha and 19 kg N/ha from plots supplied with 120 kg N/ha. The amounts of precipitation, plant growth, and N application were found to affect the denitrification rate. These factors also affected the ratio (N₂O+N₂)/N₂O, which varied from 1.0 to 7.2. Plant growth and precipitation increased the proportion of N₂ produced, whereas a high nitrate content increased the proportion of N₂O.     

The influence of sewage sludge on the content of heavy metals in potatoes and on tuber yield

Summary A small plot field experiment with two types of sewage sludge, one poor and one rich in heavy metals, applied in moderate and heavy quantities, and compared with NPK-fertilizer, was carried out 1973 and 1974, in potatoes. The chemical composition of the NPK-fertilizer and the sludges, and the amounts applied are found in Tables 1 and 2.The sludge increased the content of total Cd, Ni and Pb and the content of readily soluble Cu and Zn in the soil. The increase was greatest for Cu and Zn, and was more pronounced the second than the first year (Table 3). The small quantities of heavy metals in NPK-fertilizer did not influence the soil analytical values.Digested sludge increased the yield of tubers significantly, but based on the amounts of nutrients applied, NPK-fertilizer was much more efficient than sludge (Table 4). It is suggested that low utilization of N, or lack of K, is mainly responsible for the lower efficiency of sludge. Toxicity in the plants due to sludge was not observed.Application of 40–80 tons/ha of sludge dry matter, rich in heavy metals, increased considerably the concentration of Cu and Zn in the tubers, whereas 10–20 tons/ha did not influence the concentration (Table 6). The content of Hg, Ni and Pb in the tubers was very little influenced by sludge application. The Cd-concentration was mostly below 0.05 mg/kg of fresh tubers, and the analytical technique was not accurate enough to detect possible influence of increasing amounts of Cd in sludge. Generally, less than 0.5% of the heavy metals applied was accumulated in the tubers. The concentration of heavy metals in fresh tubers was in all cases below suggested maximum tolerable values for food. re]19760203     

Field observations on nitrogen catch crops. III. Transfer of nitrogen to the succeeding main crop

In temperate climates with a precipitation surplus during autumn and winter, nitrogen (N) catch crops can help to reduce nitrogen losses from cropping systems by absorbing nitrogen from the soil and transfer it to a following main crop. In two field experiments the catch crop species winter rye (Secale cereale) and forage rape (Brassica napus ssp. oleifera (Metzg.) Sinsk) or oil radish (Raphanus sativus spp. oleiferus (DC.) Metzg.) were planted end of August and 3 weeks later with a non-limiting supply of N and zero-N controls. In the next spring catch crops were incorporated into the soil. In Expt 1, N transfer was measured as (i) the N uptake of a potato test crop, grown with zero and 12.5 g m^–2 N applied, and (ii) the increase in soil mineral N (0–30 cm) in uncropped soil covered with polythene film. In Expt 2, N transfer was measured as the increase in soil mineral N in covered cylinders placed in uncropped soil (in situ incubation). Subsidiary laboratory incubations were performed in Expt 2. In Expt 1, the apparent recovery in potato of fertilizer N (R _f) was 0.56. The recovery in potato of N mineralized from 'native' N pools other than catch crop material (R _n) ranged from 0.43 to 0.51, depending on the value assumed for the depth of N extraction by potato roots. The average recovery in potato of incorporated catch crop N (R _c) was 0.34. Expressed as `fertilizer N replacement factor' (F _r) the latter was 0.61 (i.e. 1 kg of N in catch crop material counts for 0.61 kg fertilizer N). Under the film in Expt 1 the fraction net mineralization of incorporated catch crop N (M _n) was 0.36 on August 11 and 0.43 on October 18. In Expt 2, the average value of M _n was 0.31, which was lower than in Expt 1 and probably associated with the drier soil in Expt 2. In the laboratory incubations (20°C) M _n showed values up to 0.54 after 84 days with the largest rates of change in mineralization occuring early after the start of the incubation. In conjunction with literature data it is concluded that cultivation of nitrogen catch crops shows promise as a means to reduce N input and N losses in temperate climates with wet winters.