Effects of experimental soil moisture fluctuations on turnover rates of testacea

Experiments designed to obtain data on the quantitative effects of an artificial increase in soil moisture content during a seasonal dry period on numbers of soil Testacea were carried out in a welldrained aspen woodland soil in the Rocky Mountains of Canada. The general effect of the addition of water to the soil was to increase significantly the number of active Testacea and decrease the number of encysted forms. Numbers of active Testacea and of total living Testacea (active plus encysted forms) showed significant, positive correlation with soil moisture content. A method for the estimation of standing crop turnover and secondary production is discussed. Generation times were shorter and secondary production higher in the watered plots.     

Phosphorus in the soil microbial biomass

Phosphorus in the soil microbial biomass (biomass P) and soil biomass carbon (biomass C) were linearly related in 15 soils (8 grassland, 6 arable, 1 deciduous woodland), with a mean P concentration of 3.3% in the soil biomass. The regression accounted for 82% of the variance in the data. The relationship was less close than that previously measured between soil biomass C and soil ATP content and indicates that biomass P measurements can only provide a rough estimate of biomass C content. Neither P concentration in the soil biomass, nor the amount of biomass P in soil, were correlated with soil NaHCO₃-extractable inorganic, organic or total P.The calculated mean annual flux of P through the biomass (in a soil depth of 10 cm) in 8 grassland soils was large, 23 kg P ha^?1 yr^?1, and more than three times the mean annual P flux through 6 arable soils (7 kg P ha^?1 yr^?1), suggesting that biomass P could make a significant contribution to plant P nutrition in grassland.About 3% of the total soil organic P in the arable soils was in microbial biomass and from 5 to 24% in the grassland soils. The decline in biomass P when an old grassland soil was put into an arable rotation for about 20 yr was sufficient to account for about 50% of the decline in total soil organic P during this period. When an old arable soil reverted to woodland, soil organic P doubled in 100 yr; biomass P increased 11-fold during the same period.     

Biomass and turnover of bacteria in a forest soil and a peat

Short-term changes in numbers and biomass of bacteria, determined by direct counts, are descrived for a subarctic mire and for the humus and mineral soil layers of pine forest podsol. For biomass, monthly fluctuations for 15 months are presented. Almost as large fluctuations in bacterial numbers were found during 2 weeks as were found during the whole year. Precipitation resulted in increases in bacterial biomass even when the soil moisture content was non-limiting for bacterial growth, but these increases did not last for more than 1–2 days. Observed rapid declines in bacterial numbers were interpreted as the result of grazing by the microfuana. Changes in cell sizes and shapes after rainfall indicated that even under favourable growth conditions only 15–30% of the bacteria were active. The increases in bacterial biomass were used to calculate a minimum production. For the bacteria in the peat the production over 9 days was 40% of the mean standing crop value per day. The corresponding values for the bacteria of the humus and mineral layer over 13 days were 19 and 15%. The average generation times, estimated from increases in numbers, were 39 h for the peat bacteria and 66 and 55 h for the bacteria of the humus and mineral layers respectively. Based on the number of falls of rain a yearly bacterial production value of 210 g d.w.m^?2 was calculated for the forest site. This figure is discussed in relation to the yearly energy input through primary production.     

Microbial biomass C- and N-dynamics in grassland soils amended with liquid manure

Turnover and fluxes of C and N through microbial biomass were investigated on a research site in the grassland region of southwestern Germany. For a period of twelve months, biomass C was determined every 2 weeks and biomass N every 4 weeks (Fumigation-Extraction). This was done at fertilized plots as well as on plots, which had not been fertilized for eight years. Biomass C and N accounted for 1.5–7.5% of the soil C and 2–9% of the soil nitrogen. Unfertilized plots contained more biomass C and N than fertilized plots. No seasonal influence on the amount of the microbial biomass was visible. C/N ratios were not related to fertilization events. An increase of the C/N ratio with depth suggests a dominance of fungi in the subsurface horizons. Estimates of biomass C and N turnover were calculated by dividing the total measured losses of biomass by the average quantity of biomass present (McGill et al., 1986), annual fluxes of carbon and nitrogen were calculated by dividing annual mean C(N) by the average C(N) in biomass (Jenkinson and Ladd, 1981). Average turnover rates for biomass C varied between 1.4 and 4.5 a^?1, turnover rates for nitrogen were slower (1.2–3.3 a^?1). Carbon Ruxes through the microbial biomass range from 5000 to 8000 kg ha^?1 a^?1, while nitrogen fluxes range from 400 to 700 kg ha^?1 a^?1.     

Carbon pools and fluxes of 25-year old coniferous and deciduous stands in middle Siberia

Between 72 and 88% of carbon (C) loss in forest litter decomposition returns to the atmosphere in the form of carbon dioxide. The share of water-soluble organic products does not exceed 3–4%. Between 8% under spruce and 25% under aspen and pine of the total C loss from litter organic matter goes to the formation of humus. Decomposition intensity of the dead organic matter on the soil surface is close to annual litterfall income (except under cedar). The specific rate of decomposition processes among the coniferous litters is minimum for cedar (167 mgC g^?1yr^?1) and maximum for larch (249 mg C g^?1 yr^?1). The specific rate of decomposition of organic residues under aspen and birch canopies are 344 and 362 mg C g^?1yr^?1.     

The earthworm population of a winter cereal field and its effects on soil and nitrogen turnover

The earthworm population in a winter cereal field in Ireland was studied over a 3-year-period and its effects on soil and N turnover were assessed. The mean annual population density was 346–471 individuals m^-2 and the mean biomass was 56.9–61.2 g m^-2. Twelve species were recorded, the most abundant being Allolobophora chlorotica followed by Aporrectodea caliginosa, and 242 mg at 5°C to 713 mg at 10°C in the case of juvenile Lumbricus terrestris. Gut contents (dry mass of soil) comprised 6.7–15.5% of the A. caliginosa live mass, and 9.7–14.7% of the Lumbricus terrestris mass. Annual soil egestion by the field population was estimated as 18–22 kg m^-2. Tissue production ranged from 81.7 to 218.5 g m^-2, while N turnover resulting from mortality was calculated as 1.5–3.9 g m^-2 depending on the year and the method of calculation. Earthworms were estimated to contribute an additional 3.4–4.1 g mineral N to the soil through excretion, mucus production, and soil ingestion. Independent estimates of N output via mucus and excretion derived from ¹⁵N laboratory studies with Lumbricus terrestris were 2.9–3.6 g m^-2 year^-1.     

The impact of cultivation on carbon fluxes in woody savannas of Southern Africa

The rapid transition from miombo woodland and savanna to maize-based agriculture in Southern Africa results in a near universal loss of total system and biomass carbon. Forests and savannas occupy approximately 3.1 million km² in southern Africa. Two natural ecosystems, a miombo woodland (Zimbabwe) and a broadleafed dry savanna (South Africa), contained 48 and 94 Mg C ha^?1, respectively. Clearing of the miombo and establishment of maize-based agriculture on a sandy Alfisol resulted in a decline in total soil organic carbon from 28 to as little as 9 Mg ha^?1. This decline is not related to the annual aboveground productivities which, in many cases is greater in the cropping system than in the savanna or forest. Severe declines in total soil organic matter resulting from shifting cultivation were also observed in coastal Mozambique. The CENTURY plant/soil simulation model was used to simulate long-term carbon dynamics a miombo woodland and maize-based cropping system in Marondera, Zimbabwe. The miombo woodland continues to accumulate total system C but shifting cultivation and commercial cultivation of maize result in annual carbon losses of 0.15 and 0.14 Mg ha^?1 yr^?1. Increases in temperature (2° C) accompanied by 25% increases in photosynthetic efficiency did not effect the decline in total system carbon, however, improved organic matter management within the agroecosystem reduced the losses in total system carbon within the agroecosystem by 57% under the climate change scenario.     

不同土地利用方式对土壤微生物生物量氮的影响

研究了长期定位试验不同土地利用方式下土壤微生物生物量氮的变化,结果表明:农田生态系统中,长期施用化肥并不能提高微生物生物量氮的水平,但可以加快其周转速率。NPK配合猪厩肥处理的微生物体氮含量最高,周转也最快。林地和草地生态系统中,荒地处理由于积累的有机物很多,其微生物量氮最大,其次是林地处理和割草处理,裸地处理的微生物生物量氮最低。各处理的土壤微生物量周转速率为:NPK+M>荒地>林地=割草>NPK>CK>裸地。     

Variation of four phosphorus properties in woodland soils

Variation in total, organic and available-P contents and phosphatase activity of P-deficient soils of some English Lake District woodlands of differing vegetative composition were examined in relation to individual woodlands, two depths in the soil profile, mull, moder and mor humus types, and different times of the year. Depth in the soil profile was a more important source of variation in the P properties than different woodlands. Soils in individual woodlands differed in their degree of variability in the four P properties. Available P contents and phosphatase activities were more variable than total and organic P contents. Available-P and organic-P contents and phosphatase activity showed seasonal variation. Seasonal variation in available-P was almost as great as differences in available-P between woodlands. Total and organic-P contents showed similar patterns of variation with respect to individual woodlands, humus type and soil depth. Differences in degree of variation within woodlands and differences in degree and pattern of variation of the four P-properties may need to be taken into account in soil sampling programmes of studies comparing soils under differing vegetation regimes.Different interpretations of the variation in the soil-P properties were obtained by expressing the data respectively in terms of soil weight (g^?1 soil) or soil volume (cm^?1 soil), due to marked variation in bulk-densities of the woodland soils. It is suggested that where soils vary in bulk-density, soil data should be expressed in terms of soil volume.The P-deficiency of the woodland soils is probably associated with the relatively low total P content per unit volume of soil and the high proportion of it which is organically bound.     

Potential of the Silpho Moor experimental birch plots as a habitat for Lumbricus terrestris

It is argued that the podzol of Silpho Moor could be converted under birch to a typical brown earth only if it could sustain an earthworm population with a Lumbricus terrestris biomass of not less than 100 g m^?2. No worms of this species were found under experimental birch plots 30 yr old. The presence of podzolizing species in the ground vegetation; the low pH of the raw humus layer; the low Ca and N supply in the soil, litter and rainfall; and the impeded soil drainage lead to the conclusion that colonization by L. terrestris is unlikely.     

Effects of lignin‐modified Populus tremuloides on soil organic carbon

Several genes in the aspen genome have been modified to generate stem wood with lower lignin content and an altered lignin composition. Lower lignin in wood reduces the time and energy required for pulping. Further, this modification can also increase the allocation of photosynthate to cellulose and total biomass production, potentially increasing CO₂‐sequestration capacity. However, widespread planting of trees with altered lignin content and composition could alter soil organic‐C dynamics in complex ways. To further examine the effects of altered lignin biosynthesis on plant growth and accrual of soil organic C (SOC), we conducted a repeated greenhouse study with four lines of transgenic aspen (Populus tremuloides Michx.) and one wild‐type (control) aspen. Accrual of aspen‐derived SOC was quantified by growing aspen trees (C3 plants) in C4 soil and measuring changes in the natural abundance of δ¹³C. We measured plant growth, biomass, and C content and combined these data with SOC measurements to create C budgets for the plant mesocosms. Lignin modifications resulted in differences in the accrual of aspen‐derived SOC and total mesocosm C, primarily due to differences in biomass between genetically modified lines of aspen. One genetic alteration (low lignin, line 23) was able to perform similarly or better than the wild‐type aspen (control, line 271) without altering SOC. Alterations in lignin structure (S : G ratios) had negative effects on biomass production and SOC formation. The addition of new (aspen‐derived) SOC was proportional to the loss of existing SOC, evidence for a priming effect. The pool of new SOC was related to total plant biomass, suggesting that the effects of lignin modification on SOC are driven by changes in plant growth.     

The role of amino acids and nucleic bases in turnover of nitrogen and carbon in soil humic fractions

Incorporation of labelled ¹⁵N and ¹⁴C amino acids and nucleic bases into soil humus fractions as well as humus turnover was investigated under field conditions. The dynamics of ¹⁵N and ¹⁴C incorporation into organic matter was characterized by the following main steps: rapid incorporation of the labelled substance prevailing for the first 1–3 weeks, and decomposition of included labelled fragments prevailing beyond one month after substance addition. The annual turnover rates of N and C in humus fractions due to incorporation of amino acids and nucleic bases were calculated. The turnover rate of N in humus is two to three times that of C. The contribution of amino acids to organic matter generation is about twice as great as that of nucleic bases and other N-containing organic substances. This indicates the important role of amino acids in the humification process and humus turnover. Turnovers of humic acids (0·002 year^?1 for C and 0·02 for N) are the most rapid of humic fractions investigated, and humin is characterized by the slowest turnover (0·0002 year^?1 for C and 0·007 for N). There are no significant differences in the turnover rates of fulvic acid fractions (0·0002 year^?1 for C) with different molecular weight.     

Evaluation of a membrane filter technique to count soil and litter testacea

The millipore filtering technique, to enumerate soil Testacea (Coûteaux, 1967), was evaluated for use in testacean population studies in a cool temperate deciduous forest soil. The modifications tested were number of samples required, sample replication, and type and length of sample maceration. The millipore filtering technique was compared to the agar film technique, another direct observation technique used for the estimation of numbers of soil Testacea (Heal, 1964). The results showed that the number of species observed, the number of active and encysted Testacea and empty tests counted for each species, and the number of total Testacea were substantially greater using the millipore filtering technique.     

A survey of the forest site characteristics in a transect through the central Canadian boreal forest

As a contribution to the BOReal Ecosystem Atmosphere Study (BOREAS), a total of 97 sites have been surveyed in the boreal forest regions of Manitoba and Saskatchewan. The sites extend across an ecoclimatic transect through the boreal forest of central Canada, from aspen parkland to sub-arctic woodland. Sites were selected using satellite, air photograph, and forest cover map data. Each site represents a minimum 100 m by 100 m homogeneous stand, suitable for satellite imaging. Data collected at each site covers overstory (species composition, DBH, pathogens, age, etc.), understory (percent cover by species), debris, and soil characteristics. These data provide a background database for the diverse measurements of terrestrial ecology, land surface climatology, tropospheric chemistry, and remote sensing. Such data provide an important baseline for ongoing studies of the boreal forest in a region sensitive to global change. The results of this study aid integration of a variety of more detailed studies being carried out in the region and also allow comparison with other international studies of a similar nature. Sites are concentrated in two regions: north of Prince Albert, Saskatchewan, and west of Thompson, Manitoba. Additional sites are located in the area of the Boreal Forest Transect Case Study (BFTCS) between Batoche, Saskatchewan and Gillam, Manitoba. The surveyed sites were classified according to three criteria: dominant species (Picea mariana, Populus tremuloides, Pinus banksiana, or “mixed”), age (mature, immature, or young/recently disturbed), and productivity (low, medium, or high). Overstory and understory measurements were usually taken at three points within each site. Debris measurements were taken at two points, and soil measurements at one point per site. This paper focuses on overstory and debris data taken at 97 sites in 1993 and 1994. The sites are predominantly in medium and high productivity stands. Overstoiy. data, primarily from point-sampling, have been used to estimate stand basal areas, stem densities, volumes, and aboveground biomass (excluding foliage). Stand basal areas ranged from 5 m² ha^?1 to over 60 m² ha^?1. Stem densities ranged from a few hundred to over 40 000 stem ha^?1. Estimates of total aboveground biomass range from a few Mg ha^?1 to over 250 Mg ha^?1. The Prince Albert sites tend to have greater values than Thompson for basal area, volume and biomass, but stem densities are highly variable. Detritus data show values from zero to 60 Mg ha^?1. Generally, these values are small compared to aboveground biomass, but in recently disturbed sites the detrital mass can exceed aboveground biomass.     

Weed abundance and soil seedbank responses to tillage systems in continuous maize crops

Weed abundance in crops undergoes frequent changes, often due to changes in tillage practices. Annual species, with quick germination, a short vegetative stage, profuse seed production and long-lived seeds become problematic under zero-tillage systems. Portulaca oleracea L. and Amaranthus blitoides L. are widespread weeds in the Mediterranean area, prominent in irrigated crops. We studied the total weed abundance in the field, and specifically these two species (Portulaca oleracea and Amaranthus blitoides) with high frequency of occurrence in monoculture maize, from 2012 to 2014, in the field and soil seedbank. Results showed significant differences between zero-tillage (ZT) and conventional tillage (CT) systems on total weed abundance and relative abundance of Portulaca oleracea. Total weed abundance decreased in ZT plots (from 136 plants m^?2 to 25 and 46 plants m^?2, in 2013 and 2014 respectively). The same trend was observed in Portulaca oleracea recorded in ZT plots, but the abundance of Amaranthus blitoides did not vary in this system. Weed seedling germination and weed seed numbers both of total weed seedbank and Portulaca oleracea, were greater in ZT plots compared to CT, regarding Amaranthus blitoides seedling germination and seed count, the values did not increase with ZT, in continuous maize crops.     

Crop production impacts on soil phosphorus removal and soil test levels

An 8-year field study documented the impact of tillage, crop rotations, and crop residue management on agronomic and soil parameters at Brookings, South Dakota. The greatest annual proportion of above-ground biomass phosphorus (P) removed was from the grain (78–87% of total) although crop residue removed some P as well. Greater above-ground total biomass P (grain P + crop residue P) was removed from corn than from soybean and spring wheat crops mainly due to the greater corn grain biomass harvested. Cumulative above-ground biomass P removal was greatest for the corn-soybean rotation (214 kg P ha^?1), while it was lowest for the soybean-wheat rotation (157 kg P ha^?1). Tillage treatments within crop rotation or residue management treatments did not influence annual or cumulative P removal rates. Olsen extractable soil orthophosphate-P levels declined consistently through time from a mean of 40 µg g^?1 (2004) to 26 µg g^?1 (2011). Biomass P removal was calculated to be 15.7 ha^?1 yr^?1 to decrease Olsen extractable soil orthophosphate-P levels by 1 µg g^?1 yr^?1 over 8 years of the study.     

Primary immigration and succession of soil organisms on reclaimed opencast coal mining areas in eastern Germany

Immigration to and colonisation of recultivated opencast coal mining areas by soil organisms were investigated in eastern Germany during the period 1996–1998 in freshly exposed substrates (immigration test) and two up to 46-year-old afforested mine soils (stage-dependent succession). The results indicate that immigration by air is characteristic for protists, soil microarthropods and spiders, while active locomotion is more important for the soil macrofauna. Testate amoebae assemblages showed no evident differences between 30–37-year-old Tertiary afforestations (ash-ameliorated, pyrite-rich, low soil pH) and 46-year-old Pleistocene sites (liming, low pyrite content, moderate soil pH), while comparisons in soil animals revealed pronounced differences in abundance, biomass and species composition. Earthworms, for example, reached a mean biomass up to 108 g m^–2 in the Pleistocene deciduous afforestation. The Tertiary site had only 7–12 g m^–2. Generally, all investigated soil animal groups indicated taxon-specific immigration and colonisation strategies with pronounced site preferences, dependent on substrate quality, age and afforestation. Within 40 years, a consistent trend is visible from an open pioneer to a woodland community. Furthermore, it was demonstrated that long-term investigations as well as numerous taxa of different trophic levels are essential for a comprehensive evaluation of recultivated mine dumps.     

Population dynamics of the earthworm Amynthas alexandri (Annelida: Megascolecidae) in a Kumaun Himalayan pasture soil

Ecological studies on earthworms were conducted in a Kumaun Himalayan pasture soil. The C:N ratio in the soil declined with increasing depth. A combination of hand-sorting and formalin application was used to sample the earthworms. Three species, Amynthas alexandri, A. diffringens (Megascolecidae), and Eisenia fetida (Lumbricidae) were found. Of the 13310 individuals collected, 99.9% were A. alexandri. The maximum density (138.8 m^-2) and biomass (25.2 g m^-2) were recorded in the wet season. More than 60% of the total earthworm numbers and biomass were recorded at 0–10 cm in depth. The mean yearly ratio of clitellate to aclitellate worms was 1:7.3.     

Effect of irrigation on nematode population dynamics and activity in desert soils

Summary The nematode community in litter and soil was examined for a year in the Chihuahuan desert, before and after supplemental rainfall application. Proportions of nematode-active or anhydrobiotic forms and population densities were determined for 3 treatments: control (natural rainfall), a single, large (25-mm) monthly irrigation pulse, and 4 smaller (6-mm) irrigations spaced at weekly intervals. In litter the greatest nematode abundance was in the 6 mm week^–1 treatment (48 nematodes 20 g^–1 litter). Bacteriovores and fungivores accounted for approximately 95% of the numbers and biomass in all treatments. In soil, water amendments had no significant effect (P < 0.05) on annual mean densities of total nematodes, fungivores, bacterivores, or omnivore predators. Phytophage densities were greater on both irrigation treatments, with highest densities (9268 m^–2) in the 6 mm week^–1 soils, which was 5.9% of the total soil nematode density. Total densities of individual trophic groups were not significantly different before or after rainfall. Soil nematode densities fluctuated independently with trophic group, month, and season. Bacterial feeders and omnivore predators were the largest contributor to total soil nematode density and biomass. Prior to irrigation, there were no differences in the percentage of anhydrobiotes on the three treatments. Anhydrobiotes decreased after irrigation in all treatments, and were significantly lower in soils of the larger, monthly irrigation. Nematodes were inactive (anhydrobiotic) and decoupled from decomposition processes when soil water matric potentials reached –0.4 MPa.Dedicated to the late Prof. Dr. M.S. Ghilarov     

Maintenance carbon requirements of actively-metabolizing microbial populations under in situ conditions

For estimating turnover rates of soil microbial populations or for energy balance studies maintenance coefficients of microorganisms grown in vitro have generally been used. To study maintenance carbon requirements under in situ conditions the biomasses of two agricultural soils (Cambisol, Chernozem) and a beech forest soil (Rendzina) were activated metabolically and the CO₂ production rate at 22°C recorded every hour. In soil samples treated with increasing amounts of glucose the concentration was determined that still yielded a maximal initial respiratory response but where the CO₂ rate remained constant over 8–13 h. Decrease of CO₂ production after that time was directly related to glucose exhaustion. The amount of glucose-C which kept the CO₂-C rate at the previous level was regarded as the maintenance ration. Values for the maintenance coefficient m (mg glucose-C mg^?1 biomass-C) were 0.012 h^?1 for the two agricultural soils and 0.03 h^?1 for the forest soil. The metabolic quotient qCO₂ and maintenance values were identical for both agricultural soils and the qCO₂ values were the same in the three soils used. No net growth was observed during the experimental period using bacterial plate counts and nalidixic acid treatment as test measurements.The determined m values reflect all individual maintenance requirements of species belonging to the total active biomass pool in these particular soils and correspond to known values from in vitro studies. The relationship between annual input of carbon and the maintenance requirements of actively-metabolizing biomasses are discussed.