The influence of moisture and temperature on the number of microorganisms in the soil

Folia Microbiologica - The influence of moisture and temperature on the number of bacteria in the soil was studied by means of Strugger’s microscopic fluorescence method. Field and laboratory...     

The influence of the soil structure and moisture content on the number of bacteria and the degree of nitrification

ИзгчалоAЬ одноврeмeнноe дeйствиe сBрCкСC@ы поGвKi и Aодeрeа влаBи на количe бактeрий и интeнсивноAтЬ нитрифика. ции в гумуA-карбонаBной почвe. Путeм просeиваниHя образцоCпочвы чeрeз сиBа были в044B;цeлeны слeдующиe фракции: I — агрeгaаты мeнЬшe 1 мм; II — агрeгаты размe@ами в 1—2; мм; III — аг@eгаты размeрами в 2—3 мм; IV — агтeгаBы размeрами в 3—4 мм; V — агрeгаBы размeрами в 4—5 мм. Образцы брали три @аза а год. Для опрeДeлeния количeства бактeрий полЬзовалисЬ прямым мeтодeм флуорeсцeнтной м0438;H043A;H0440;H043E;скопии по Strugger в модификации по Seifert. Пeрeд опрeдeлeниeм биогeнности образцы насыщли влагой до заранee установлeнного уровня и инкCбировали 48 час. при тeмпeратгрe 20° С Нитрификацию опрeдeлOли послe 14-днeвной ?нкгбации образFов, насKщeнных влвгой до опрeдeлeнного уровня и хранившихся в тeрмостатe пр? 20° А. Бы;ло установлeно, что количeство бактeрий зависит от содeржания влаги и 043F;очти нe зависит оB размeров агрeгатов (рис. 1). ИнтeнсивностЬ нитрификации зависит как от содeржаниO влаги, так ? оB размeров агр;eгатов. НаиболЬHая интeнсивностЬ наблюдаласЬ в слу чаe агрeгатов пe@вой фракции, т. e. при диамeтрах мeнЬHe 1 мм. С гвeличeниeм диамeтров агрeгатов интeнсивностЬ нитрификации постeпeнно поннжаласЬ (@ис. 2). Понижeниe интeнсивности нитрификации отличалосЬ опрeдeлCнной правилЬностЬю, инаосновании ee анализа мы пришли к выводу, что инBeнсивностЬ нитрификаFии прямо пропорFионадЬна вeдиGинe спeцифичeAкой повeрхносBи агрeгатов. ДоказатdдЬство зтого привeдeно на рис. З. Для протeрки того, как на интeнсивносBЬ нитрификации дeйствуeт радмeлЬчeниe агрeгатов, мы поставнди опыт, при котором апрeгаBы V фракции были размeлЬчeны до размeров I фракции. Послe измeлЬчeниO интeнсивностЬ ниBририкаFии знаGиBeлЬно повысиласЬ (рис. 4).     

The influence of moisture regimes on the population and activity of soil microorganisms

This paper deals with the influence of soil moisture on the fungal population, bacterial population, CO₂-evolution and dehydrogenase activity. Correlation coefficients of various parameters of the soil with different moisture regimes are given. It is demonstrated that soil moisture significantly alters the microbial population, its activity and the relationships between various parameters.     

The influence of soil moisture on losses of buried seeds to fungi

Although soil fungi are likely to be a major cause of mortality for buried seeds, few ecological studies have examined the role these pathogens play in natural systems. In particular, few studies have investigated whether losses of seeds to soil fungi are habitat-dependent. We used fungicide treatments to investigate whether losses of buried seeds of four grasses (Bromus inermis, Danthonia spicata, Glyceria striata, and Poa pratensis) to soil fungi differed among meadows differing in soil moisture. We also applied water to some treatments, to determine whether this increased losses of seeds to fungi. For all four grasses, fungicide additions improved one or more measures of seed viability, though this effect was small. For Danthonia and Glyceria, fungicide was less likely to improve viability in dry meadows than in wet and/or mesic meadows. Adding water reduced some measures of viability of seeds of Danthonia and Poa in dry meadows, but fungicide partly counteracted these negative effects, suggesting that adding water reduced performance by increasing fungal attack. These results indicate that fungi represent a hazard for buried seeds of these species, particularly in wetter soils, and potentially may contribute to the reduction of populations of vulnerable species in wetter sites.     

Microbial soil respiration and its dependency on carbon inputs, soil temperature and moisture

This experiment was designed to study three determinant factors in decomposition patterns of soil organic matter (SOM): temperature, water and carbon (C) inputs. The study combined field measurements with soil lab incubations and ends with a modelling framework based on the results obtained. Soil respiration was periodically measured at an oak savanna woodland and a ponderosa pine plantation. Intact soils cores were collected at both ecosystems, including soils with most labile C burnt off, soils with some labile C gone and soils with fresh inputs of labile C. Two treatments, dry‐field condition and field capacity, were applied to an incubation that lasted 111 days. Short‐term temperature changes were applied to the soils periodically to quantify temperature responses. This was done to prevent confounding results associated with different pools of C that would result by exposing treatments chronically to different temperature regimes. This paper discusses the role of the above‐defined environmental factors on the variability of soil C dynamics. At the seasonal scale, temperature and water were, respectively, the main limiting factors controlling soil CO₂ efflux for the ponderosa pine and the oak savanna ecosystems. Spatial and seasonal variations in plant activity (root respiration and exudates production) exerted a strong influence over the seasonal and spatial variation of soil metabolic activity. Mean residence times of bulk SOM were significantly lower at the Nitrogen (N)‐rich deciduous savanna than at the N‐limited evergreen dominated pine ecosystem. At shorter time scales (daily), SOM decomposition was controlled primarily by temperature during wet periods and by the combined effect of water and temperature during dry periods. Secondary control was provided by the presence/absence of plant derived C inputs (exudation). Further analyses of SOM decomposition suggest that factors such as changes in the decomposer community, stress‐induced changes in the metabolic activity of decomposers or SOM stabilization patterns remain unresolved, but should also be considered in future SOM decomposition studies. Observations and confounding factors associated with SOM decomposition patterns and its temperature sensitivity are summarized in the modeling framework.     

Calibration of Watermark soil moisture sensors for soil matric potential and temperature

Rapid, accurate, and automated measurement of soil matric potential is desirable. Evidence suggested that the Watermark resistance block might be an appropriate and inexpensive tool, so we conducted an evaluation of its relevant characteristics. A number of these blocks were calibrated under laboratory conditions to determine their individual and aggregate responses to soil matric potential, soil type, and temperature. We found that the temperature response could be expressed as a single equation, valid for all tested blocks, but comparison against matric potential revealed that each block had a characteristic response. Furthermore, block responses were different in two soils and, for a given soil, not necessarily reproducible. Given these limitations, these sensors are probably useful only as relative indicators of soil water status.     

Effects of soil phosphorus availability,temperature and moisture on soil respiration in Eucalyptus pauciflora forest

Rates of soil respiration (CO₂ efflux) were measured for a year in a mature Eucalyptus pauciflora forest in unfertilized and phosphorus-fertilized plots. Soil CO₂ efflux showed a distinct seasonal trend, and average daily rates ranged from 124 to 574 mg CO₂ m^–2 hr^–1. Temperature and moisture are the main variables that cause variation in soil CO₂ efflux; hence their effects were investigated over a year so as to then differentiate the treatment effect of phosphorus (P) nutrition.Soil temperature had the greatest effect on CO₂ efflux and exhibited a highly significant logarithmic relationship (r² = 0.81). Periods of low soil and litter moisture occurred during summer when temperatures were greater than 10 °C, and this resulted in depression of soil CO₂ efflux. During winter, when temperatures were less than 10 °C, soil and litter moisture were consistently high and thus their variation had little effect on soil CO₂ efflux. A multiple regression model including soil temperature, and soil and litter moisture accounted for 97% of the variance in rates of CO₂ efflux, and thus can be used to predict soil CO₂ efflux at this site with high accuracy. Total annual efflux of carbon from soil was estimated to be 7.11 t C ha^–1 yr^–1. The model was used to predict changes in this annual flux if temperature and moisture conditions were altered. The extent to which coefficients of the model differ among sites and forest types requires testing.Increased soil P availability resulted in a large increase in stem growth of trees but a reduction in the rate of soil CO₂ efflux by approximately 8%. This reduction is suggested to be due to lower root activity resulting from reduced allocation of assimilate belowground. Root activity changed when P was added to microsites within plots, and via the whole tree root system at the plot level. These relationships of belowground carbon fluxes with temperature, moisture and nutrient availability provide essential information for understanding and predicting potential changes in forest ecosystems in response to land use management or climate change.     

The influence of soil moisture and flooding on formation of VA-endo- and ectomycorrhizae in Populus and Salix

Native mixtures of extomycorrhizal fungi were found to infect Populus and Salix roots primarily in very moist but well drained soils in both the field and in controlled experiments (0 to –0.2 MPa), whereas native mixtures of VA-endomycorrhizal fungi infected roots over a much wider range of soil moisture (flooded to –3.4 MPa). Although a moisture gradient experiment showed endomycorrhizal formation was greater in moist soil than in very dry or flooded soils, this pattern was reversed in field transects along drainage gradients. Infection by VA-endomycorrhizal fungi in the field was the lowest where infection by ectomycorrhizal fungi was high, which suggests possible antagonism among the fungal symbionts. The narrow moisture range for ectomycorrhizal formation, and antagonism among endo- and ectomycorrhizal fungi, apparently combine to produce the mycorrhizal distributions found in nature.     

Improving grasslands: the influence of soil moisture and nitrogen fertilization on the establishment of seedlings

1. In order to investigate the factors influencing the establishment of seedlings in permanent grassland, the influence of soil moisture and nitrogen fertilization on competition between established plants of Lolium perenne and seedlings of Phleum pratense or Trifolium pratense was studied in two experiments under greenhouse conditions using the 'split-box'-technique.
2. There was no difference in the production of plant dry matter of P. pratense or T. pratense between 30% volumetric soil water content (−0·005 MPa) and 22% (−0·04 MPa), but 15% soil moisture (−0·33 MPa) reduced plant growth. L. perenne yields were linearly reduced by reduced soil moisture content.
3. Shoot competition from L. perenne reduced the plant dry matter yield of P. pratense and T. pratense more than did root competition in these experiments. When shoot competition was present, differences between moisture contents were not detected, indicating that light was probably the limiting resource under such conditions. No significant interaction between root competition and soil moisture was observed for plant weight.
4. Root competition was not prevented even though sufficient water and nitrogen were supplied. This indicated either that some other growth factor was limiting or the plants competed for resources at the root hair level even though sufficient resources were supplied at the pot or field scale. Therefore, in the situation of direct drilling of species during grassland renovation, it may be difficult to alleviate competition by adequate provision of water and nitrogen.     

The influence of soil moisture and some soil physical factors on the ovipositional behavior of the prairie grain wireworm, Ctenicera destructor

Soil moisture, texture, cracks and compaction all influenced the ovipositional behavior of Ctenicera destructor. In oviposition choice-chambers, most eggs were laid in soil with a range of moisture content about halfway between the field capacity and the permanent wilting percentage. In cylinders of soil, beetles usually burrowed to reach moist soil before ovipositing, but laid close to the surface, if the soil within 2 cm of the surface was moist and the underlying soil was dry. Soil cracks enhanced oviposition and increased the survival time of beetles in field cages. Beetles were unable to penetrate field soil unless a crack was present.Eggs laid under natural conditions were found under soil lumps in a cultivated field and under partially dried cow manure in pastures.

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Zusammenfassung Bodenfeuchtigkeit, Struktur, Verdichtung und Spalten beeinflußten das Eiablageverhalten von C. destructor. Bei Wahlkammer-Versuchen im Laboratorium reagierten die Käfer in einer Reihe von Bodenfeuchtigkeitsstufen etwa halbwegs zwischen dem permanenten Welke-Prozentsatz und der Feldkapazität. Die Tiefe der Eiablage wurde ebenfalls von der Bodenfeuchtigkeit beeinflußt. In Zylindern mit Bodenfüllung begannen die Käfer so lange nicht mit der Eiablage, bis sie in Berührung mit einer feuchten Bodenschicht kamen.Nahe der Bodenoberfläche erfolgten Eiablagen besonders dann, wenn die Bodenoberfläche feucht und der darunter liegende Boden trocken war.Die Tiefe der Eiablage im Boden wurde in Feldkäfigen von der Verdichtung und von Spalten beeinflußt. Die Lebensdauer der Weibchen und deshalb das Gesamtgelege waren um so größer die Tiefe der Spalten wurde, sowohl in gesiebten wie in ungestörten Feldböden.Unter natürlichen Bedingungen wurden ablegende Weibchen und Eigelege in einem Kulturfeld unter dem Schutz von Bodenklumpen und auf Weiden unter teilweise getrocknetem Kuhdung gefunden. Solche Art der Bodenbedeckung bietet sowohl Käfern wie Eiern Schutz und dürfte einen wichtigen Eiablageplatz im Freiland darstellen.

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Contribution No. 273, Canada Agriculture Research Station, Saskatoon, Saskatchewan     

Effects of soil moisture content and temperature on methane uptake by grasslands on sandy soils

Aerobic grasslands may consume significant amounts of atmospheric methane (CH4). We aimed (i) to assess the spatial and temporal variability of net CH4 fluxes from grasslands on aerobic sandy soils, and (ii) to explain the variability in net CH4 fluxes by differences in soil moisture content and temperature. Net CH4 fluxes were measured with vented closed flux chambers at two sites with low N input on sandy soils in the Netherlands: (i) Wolfheze, a heather grassland, and (ii) Bovenbuurtse Weilanden, a grassland which is mown twice a year. Spatial variability of net CH4 fluxes was analysed using geostatistics. In incubation experiments, the effects of soil moisture content and temperature on CH4 uptake capacity were assessed. Temporal variability of net CH4 fluxes at Wolfheze was related to differences in soil temperature (r2 of 0.57) and soil moisture content (r2 of 0.73). Atmospheric CH4 uptake was highest at high soil temperatures and intermediate soil moisture contents. Spatial variability of net CH4 fluxes was high, both at Wolfheze and at Bovenbuurtse Weilanden. Incubation experiments showed that, at soil moisture contents lower than 5% (w/w), CH4 uptake was completely inhibited, probably due to physiological water stress of methanotrophs. At soil moisture contents higher than 50% (w/w), CH4 uptake was greatly reduced, probably due to the slow down of diffusive CH4 and O2 transport in the soil, which may have resulted in reduced CH4 oxidation and possibly some CH4 production. Optimum soil moisture contents for CH4 uptake were in the range of 20 – 35% (w/w), as prevailing in the field. The sensitivity of CH4 uptake to soil moisture content may result in short-term variability of net atmospheric CH4 uptake in response to precipitation and evapotranspiration, as well as in long-term variability due to changing precipitation patterns as a result of climate change.     

The influence of soil temperature on the nesting cycle of the halictid bee Lasioglossum malachurum

The physiology and behavior of ectothermic organisms is strongly influenced by temperature. For ground nesting species like the primitively eusocial halictid bee, Lasioglossum malachurum, soil temperature might influence the life cycle as well as the complexity of the social group since the number of broods that can be fitted into the flight season might increase with increasing temperature. Our study populationof L. malachurum at Wuerzburg exhibits a remarkable variability with respect to the number of broods and the pattern of sexual production. Broods are separated by activity pauses during which the larvae develop. In this study we investigate the influence of soil temperature on the pattern of nesting activity (duration of broods and pauses) and on the number of broods in L. malachurum. We observed a total of 1138 nests in 13 aggregations near Wuerzburg. As expected, soil temperature shortened the duration of the pauses, resulting in an overall shortening of the nesting cycle. This is most probably due to a physiological effect of soil temperature on the development of the larvae. With regard to the nesting strategies, we hypothesized that a shortening of the nesting cycle within the limited flight season should enhance the success of a strategy with more worker broods. In fact, patches with higher soil temperature showed more broods. However, this effect was rather weak, suggesting that other factors might have a stronger impact on the variability in nesting strategy within our study population of L. malachurum. Received 20 December 2005; revised 25 April 2006; accepted 2 May 2006. An erratum to this article is available at .     

Effect of temperature and soil moisture content on the colonization of the wheat rhizosphere by antiphytopathogenic bacilli

Vegetative experiments showed that the population density of antiphytopathogenic bacillar species introduced into the rhizosphere of spring wheat seedlings essentially depended on the soil temperature and not on the soil moisture content. As a rule, the population of introduced bacilli increased with the temperature. Under both low and optimal soil moisture contents, introduced bacilli were efficiently acclimated in the wheat rhizosphere.     

Response of soil respiration to soil temperature and moisture in a 50-year-old oriental arborvitae plantation in China

China possesses large areas of plantation forests which take up great quantities of carbon. However, studies on soil respiration in these plantation forests are rather scarce and their soil carbon flux remains an uncertainty. In this study, we used an automatic chamber system to measure soil surface flux of a 50-year-old mature plantation of Platycladus orientalis at Jiufeng Mountain, Beijing, China. Mean daily soil respiration rates (R(s)) ranged from 0.09 to 4.87 μmol CO(2) m(-2) s(-1), with the highest values observed in August and the lowest in the winter months. A logistic model gave the best fit to the relationship between hourly R(s) and soil temperature (T(s)), explaining 82% of the variation in R(s) over the annual cycle. The annual total of soil respiration estimated from the logistic model was 645±5 g C m(-2) year(-1). The performance of the logistic model was poorest during periods of high soil temperature or low soil volumetric water content (VWC), which limits the model's ability to predict the seasonal dynamics of R(s). The logistic model will potentially overestimate R(s) at high T(s) and low VWC. Seasonally, R(s) increased significantly and linearly with increasing VWC in May and July, in which VWC was low. In the months from August to November, inclusive, in which VWC was not limiting, R(s) showed a positively exponential relationship with T(s). The seasonal sensitivity of soil respiration to T(s) (Q(10)) ranged from 0.76 in May to 4.38 in October. It was suggested that soil temperature was the main determinant of soil respiration when soil water was not limiting.     

Habitat selection and offspring survival rate in three paracoprid dung beetles: the influence of soil type and soil moisture

Paracoprid dung beetles build brood chambers in the soil beneath a dung pat and provide them with dung Onthophagus species lay one egg into each chamber This paper deals with the influence of soil type and soil moisture on micro-habitat selection and survival of offspring m three middle-European Onthophagus-species ( O coenobita, O fracticonis and O vacca) Discrimination between sandy soils with three different loam contents (0%, 20%, 40%) and four different water contents (4%, 8%, 12%, 16%) was tested in the laboratory During the first 24 h of each replicate beetles which colonized one of the patches did not distinguish between different soil conditions Emigration rates, measured as time when 50% of all individuals had left the patch, and numbers of brood chambers proved to be species specific and depended on soil moisture and soil type Survival rates of the larvae in the brood chambers were influenced nearly exclusively by soil moisture The results are discussed in relation to the ecology of the three species and in context with optimal foraging theories