岩溶区不同恢复阶段檵木根际土壤生态化学计量学特征

[目的]探讨不同植被恢复阶段中檵木(Loropetalum chinense)根际土壤生态化学计量学特征,揭示岩溶石漠化区不同恢复阶段下檵木养分利用规律及限制因子,为岩溶区植被恢复与重建提供科学依据。[方法]利用生态化学计量学方法,分析桂西北岩溶区不同植被恢复阶段(灌木林、原生林)檵木根际土壤生态化学计量学特征。[结果]檵木根际土壤C、N、P含量表现为灌木林阶段高于原生林阶段,而C∶N,C∶P,N∶P比值则刚好相反;同一植被恢复阶段,不同坡位间檵木根际土壤C∶P与N∶P比值存在显著差异;相关性分析表明,土壤C含量与土壤N∶P含量存在显著正相关关系,土壤N,P均与C∶N,C∶P,N∶P存在显著正相关关系,土壤C∶P与C∶N,N∶P存在显著正相关关系。[结论]檵木根际养分供应状况与其生境密切相关,在植被恢复前期(灌木林)檵木生长容易受N素限制,到植被恢复后期檵木生长易受P素限制。     

Effect of fertilization and irrigation upon NPK composition of corn leaves,on corn yields,and available k in soil

Abstract

Corn (Zea mays L.) was grown for three consecutive years on Congaree loam to measure the effects of rates of N, P, and K fertilization and irrigation on the nutrient concentration of leaves, the level of available K in the soil, and on the yield of corn. Plant nutrients consisting of 0, 56, 140, 224, and 280 kg N/ha; 0, 15, 37.5, 60, and 75 kg P/ha, and 0, 28, 70, 112, and 140 kg K/ha were applied in a central composite rotatable design in each of the three years. All plant residue was removed each year when the corn was harvested, and the plots remained fallow during the winter months. One half of the experiment was irrigated when there was a 50% depletion of available soil moisture in the 0‐ to 46‐cm soil depth.

Leaf composition was affected by fertilization and irrigation. A rapid decrease in available soil K in the 0‐ to 15‐cm depth was evident the first year with all rates of added K. The decline in available soil K was unaffected by irrigation and levels of applied N and P.

There were consistent yield responses each year to added N, no response to added P, and a response to added K only during the second year.     

Coupling among applied,soil, root,and top components for forage crop production

Abstract

This analysis establishes linkage among (a) applied nutrients nitrogen (N), phosphorus (P), and potassium (K), (b) available soil nutrients, (c) root dry matter and nutrient content, (d) top dry matter and nutrient content, and (e) leaf area and carbon dioxide (CO₂) concentration. It was previously shown that (a) and (d) are coupled by logistic equations with a common response coefficient c between dry matter and plant nutrient uptake with each applied nutrient. As a consequence of the common c, it has been shown that dry matter and plant nutrient removal are coupled by a hyperbolic equation. Furthermore, a model has been developed which includes N, P, and K as inputs. In the present work, (a) and (b) were coupled by a logistic equation as were (a) and (c). It was then shown that plant nutrient removal was coupled to available soil nutrients through a hyperbolic equation. The hyperbolic relationship was also shown to link dry matter between roots and tops, as well as plant N removal between roots and tops. As a consequence of the results above, it was then concluded that root nutrient content is related to available soil nutrient through a hyperbolic equation. The detailed mechanism of this coupling was not identified. Leaf area of soybeans followed a hyperbolic relationship with CO₂ concentration in the canopy.     

Establishment of soil solution P levels for studies involving vesicular‐arbuscular mycorrhizal symbiosis

Abstract

A phosphorus sorption curve was developed to evaluate the influence of established levels of soil solution P on the development of vesicular‐arbuscular mycorrhizal (VAM) activity in Leucaena leucocephala (Lam.) de Wit grown on soil:sand mixture. The P sorption curve developed after nutrient amendment and wetting and drying treatments in the greenhouse predicted levels of P established in the soil solution more accurately than P sorption isotherm developed in the laboratory.

VAM activity measured in terms of P content of pinnules of Leucaena was significantly higher at lower soil solution P levels (0.01 and 0.02 mg/L) than at higher levels. In general, VAM activity declined after reaching a peak value at 30 days after planting (DAP).

Soil solution P levels monitored during the course of the experiment indicated that low initial P levels (0.01 and 0.02 mg/L) were readily maintained than higher ones. The proposed approach is thus appropriate for establishing soil solution P levels that permit optimal VAM activity.     

Nutrient status of apple orchards in Canterbury,New Zealand. 1. Levels in soil,leaves and fruit and the prevalence of storage disorders

Abstract

The nutrient status (N, P, K, Ca, Mg, K, Fe, Mn, Zn and Cu) of 26 Cox's Orange Pippin and 20 Braeburn apple orchard sites in the Canterbury region of New Zealand was evaluated by soil, leaf and fruit analysis. Concentrations of available nutrients in soils ranged widely but those in leaves and fruit were generally confined to a relatively narrow range. Concentrations of leaf N were high in the study area, as were levels of extractable soil P, and it is suggested that reductions in fertilizer additions of these nutrients would generally be appropriate.

Soil, leaf and fruit nutrient contents were generally not well correlated with one another. The only highly significant correlations (P≤0.001) were between leaf and fruit Ca for Cox's and soil and fruit Mg for Braeburn. The poor correlations were attributed to the empirical nature of soil tests, the presence of large nutrient reserves within the tree framework and the effects of cultural and environmental factors on nutrient uptake and translocation by the trees.

The storage disorders bitter pit and senescent breakdown in Cox's and lenticel blotch pit in Braeburn were observed in apples harvested from some of the study sites. Such disorders were generally associated with low concentrations of Ca (≤.2.5 mg/100 g) in samples of cortical plugs taken from fruit at harvest.     

Nutrient status of potato grown on fine sandy loams in Prince Edward Island

Abstract

Potato (Solanum tuberosum L.) leaf tissue and corresponding soil samples were taken from 64 fields in 1988 on Prince Edward Island (P.E.I.) to characterize their nutrient status. The pH of the soil samples ranged from 4.4 ‐6.3 with a mean of 5.2. The phosphorus (P), potassium (K), magnesium (Mg), copper (Cu), zinc (Zn), boron (B), and iron (Fe) in leaves and soils were present in adequate quantities for normal potato production. Plant sulfur (S) was considerably lower in this survey than levels obtained in 1979. Leaf tissue manganese (Mn) concentrations ranged to toxic levels and were negatively correlated with soil pH. A number of leaf tissue samples tested deficient in S and low in Ca. Potato and possibly other crops may benefit from S fertilization on P.E.I.     

Production of Chinese cabbage in relation to nitrogen source,rate, and leaf nutrient concentration

Abstract

Chinese cabbage (Brassica rapa L. Chinensis group) production is expanding in the U. S., and guidelines regarding its production under Western cultural practices are needed. The objectives of this study were to investigate the effects of N source and rate on Chinese cabbage yield, marketability, and wrapper leaf nutrient concentrations, and to estimate the critical wrapper leaf‐N concentration associated with maximum yield and marketability. Chinese cabbage was grown in five sequential plantings using raised‐bed, polyethylene mulch culture with subsurface irrigation on a sandy soil. Nitrogen fertilizer was applied at rates of 0, 67,112, and 157 kg/ha using the following sources: 1) ammonium nitrate. 2) calcium nitrate, 3) urea‐ammonium nitrate solution (Uram, 32% N), 4) urea, and 5) a urea‐calcium solution (18% N). Mature Chinese cabbage wrapper leaf concentrations of P, Ca, and Mg increased with increasing N rate, while leaf‐K concentration decreased. Leaf‐N concentration increased in response to N rate, but was not affected by N source or harvest date. Leaf‐P, K, Mg, and B concentrations were sufficient or high according to established standards, but leaf‐Ca was low. Leaf‐Ca and Mg concentrations were lowest with N sources containing only urea, and highest where at least part of the N was applied as NO₃ ^‐. Chinese cabbage head weight and percentage marketable heads increased as N rate increased. Yield and quality were highest with N sources which contained NO₃ ^‐, and were smallest where N was applied entirely as urea, which may have been due to plant sensitivity to NH₄ ⁺. The critical value of mature cabbage wrapper leaf‐N concentration above which yield or marketability was not limited was estimated to be 36 to 41 mg/g, which agrees well with established standards.     

Microsite assessment of forest soil nitrogen,phosphorus, and potassium supply rates in‐field using ion exchange membranes

Abstract

A new method for microsite assessment of soil nutrient supply in forest soil was developed. The method involves the use of ion exchange membranes to assess differences in soil nitrogen (N), phosphorus (P), and potassium (K) supply rates in‐field over small depth increments in the forest floor (i.e., the L, F, and H horizons). Ion exchange membranes were buried and retrieved from the forest floor in an aspen forest stand in Saskatchewan, Canada. Small (6 mm diameter) sections of the membrane were cut out and ion concentration on the sections measured to provide a nutrient supply rate at that location. Soil nutrient supply rates at the site ranged from 4.6–6.0, 7.3–8.5, 11.6–21.5, and 122–196μg 10 cm²#lb2 h^‐1 for NH₄ ⁺‐N, NC₃ ^‐‐N, P, and K, respectively. On average, the highly humified H horizon had the highest N and P supply rates, followed by the F horizon, with the surface litter (L horizon) having the lowest N supply rates. The simplicity and sensitivity of the procedure make this method appropriate for in‐field assessment of differences in soil nutrient supply over small vertical and horizontal distance and was especially appropriate for the forest floor horizons in forest soils.     

Impacts of prescribed burnings on litter production,nitrogen concentration, δ13C and δ15N in a suburban eucalypt natural forest of subtropical Australia

Purposes

Prescribed burning is projected to be adopted more frequently with intensifying climate change; thus, a long-term study is necessary to understand the burning impacts on forest productivity and carbon (C) and nitrogen (N) cycling. Litter fall production rate can be used to indicate burning impacts on forest productivity, whereas N concentration, and C and N isotope composition (δ¹³C and δ¹⁵N) can be used to infer burning impacts on C and N cycling in plant-soil system.

Materials and methods

In this study, the impacts of low-intensity prescribed burning on litter production, N concentration, and C and N isotope compositions were continuously investigated for 6 years at five study sites in a natural eucalypt forest of subtropical Australia.

Results and discussion

Higher leaf litter production rate, N concentration and δ¹⁵N, and lower δ¹³C could be seen shortly after prescribed burning. The higher leaf litter N concentration and lower δ¹³C were likely due to the ease of competition for soil N and moisture from understory vegetation in the short term by prescribed burning. Leaf δ¹⁵N and N concentration were closely correlated, and seasonal changes in leaf litter production rate, δ¹³C and δ¹⁵N were observed. Burning season and related severity might determine the suppression degree of understory vegetation. Time since fire (TSF) was a significant impact factor influencing the litter fall production rate, N concentration, δ¹³C and δ¹⁵N of leaf litter fall for a decade following prescribed burning. However, monthly rainfall and temperature were less consistent in their impacts.

Conclusions

Nitrogen limitation was enhanced by prescribed burning through the removal of litter and understory vegetation in the N poor forest and might be responsible for the long-term burning impacts. Low-intensity prescribed burning might have a long-lasting impact on forest litter productivity in nutrient poor forests in subtropical Australia.

     

Beneficial effects of glycine on growth and leaf nutrient concentrations of coriander (Coriandrum sativum) plants

Abstract

In this study, the effect of glycine amino acid was evaluated on growth characteristics and nutrient uptake of coriander plants under greenhouse conditions. The treatments were soil application of glycine in two concentrations of 300 and 600?mg kg^?1 soil, foliar application of glycine (in 0.05% concentration), soil application of mix NPK fertilizer and no fertilizer control. The growth parameters of plant height, leaf SPAD value, shoot and root fresh weights were significantly improved by soil application of glycine, particularly in higher concentration. Soil application of glycine also reduced the number of flowered plants, while it increased soluble solids (TSS) and vitamin C of plant leaf extracts than control plants. Leaf nutrient concentrations of nitrogen (N), calcium (Ca), potassium (K), phosphorus (P), iron (Fe), and zinc (Zn), but not magnesium (Mg) and manganese (Mn), were significantly increased by soil application of glycine, whereas soil applied NPK significantly increased P and Ca of leaves than unfertilized control plants.     

The effect of vesicular-arbuscular mycorrhizal inoculation on nutrient uptake and yield of alley-cropped cassava in a degraded Alfisol of southwestern Nigeria

Leaf and root (tuber) nutrient uptake patterns of cassava (Manihot esculenta Crantz) alley-cropped with gliricidia (Gliricidia sepium), leucaena (Leucaena leucocephala), and senna [(Senna (syn. Cassia) siamea] as influenced by vesicular-arbuscular mycorrhizal (VAM) inoculation in a degraded Alfisol were investigated in consecutive years. The cassava plants were mulched with fresh prunings of each hedgerow tree species at 2-month intervals in the second and third years of alley cropping. While VAM inoculation significantly influenced the root uptake of nutrients, the leaf uptake was not affected except for the uptake of P. In most cases, there was no difference in the nutrient concentration between inoculated and uninoculated plants, either in the leaf or in the root, indicating that the productivity of cassava was regulated by the amount of nutrients the roots could absorb. In spite of similar total soil N in all inoculated and uninoculated alley-cropped cassava plots and similar exchange-able soil K contents in inoculated and uninoculated alley-cropped cassava plots with leucaena and senna, greater uptake of N, P, and K and greater concentrations of K were observed in roots of inoculated alley-cropped cassava with gliricidia and leucaena than with senna. These results indicated that greater mineralization and availability of nutrients to cassava roots from prunings of nodulating gliricidia and leucaena than from non-nodulating senna may be important, particularly with efficient VAM inoculation, in these alley-cropping systems. Also, for similar nutrients in the inoculated and uninoculated cassava soils alley-cropped with each hedgerow species, VAM inoculation significantly enhanced cassava root dry weights, indicating that an effective VAM fungus can be an agent of greater nutrient uptake in a competitive environment.     

Identification of nutritional and environmental factors affecting sugarcane production in barbados

Abstract

Sugarcane production in Barbados has declined since the 1950s. Plant nutrition and fertilization deficiencies are generally believed to negatively influence yields in Barbados. The objective of this study was to identify nutritional and environmental factors related to sugarcane yields. Leaf analyses, respective crop yields, and other data were collected from the Barbados Sugar Industry Ltd. during the period 1985–1990. The database was constructed from 2,853 site observations, consisting of crop cane yield (Mt/ha), soil grouping, ecological grouping, growing elevation, and leaf tissue analysis [nitrogen (N), phosphorus (P), potassium (K)]. Simple mean separation and tree‐based regression were used to identify nutritional and environmental factors associated with sugarcane yields. Twenty‐three environments were delineated by tree‐based regression, in which plant nutrient deficiencies (i.e., yield limiting) were identified. One environment described N‐deficient conditions, four environments described P‐deficient conditions, and five environments described K‐deficient conditions. Different critical leaf nutrient concentrations were related to yields. A single nutrient norm under different environments may be misleading. If current fertilizer recommendations are adhered to by growers in Barbados, attention to additional fertilization should be given only under these environments.     

Effect of nitrogen,phosphorus and potassium on yields,protein cohtents and otrient levels in soybeans,field peas and fababeans

Abstract

Soybeans, Glycine max (L.) Merr., field peas, Plsum sativum I., and fababeans, Vicia faba L., were each grown at either three or four locations. Fertilizer treatments consisted of three rates of N, three of P and three of K applied in all possible combinations.

In general fertilizers had minimal effects on yields and on the percentages of N, P, K, Ca and Mg in leaf tissue. The most consistent effect was a decrease in leaf Mg with application of increasing; rates of K.

Average yields at different locations ranged from 1735–2997 kg/ha for soybeans, 2940–3246 kg/ha for field peas and 1569—4435 kg/ha for fababeans. The results suggest, however, that factors other than soil chemical properties probably had an appreciable effect on yields.     

Variation within sunflower cultivars and inbred lines in leaf chemical composition

Abstract

Plant species, as well as cultivars within species, have been shown to vary in response to soil nutrient levels due to variation in tissue requirements and variation in ability to absorb nutrients from the soil. In order to study this latter aspect in sunflowers (Helianthus annuus L.), two field trials were conducted in which nutrient concentrations in the topmost nature leaf were determined. At two growth stages, 16 cultivars differed significantly in leaf nutrient levels of N, K, Ca, Mg, Mn, Cu, Zn, and B. Seed yields were highly significantly correlated with leaf nutrient levels, variation in nutrient concentrations accounting for 43% of the observed variation in seed yield. On this soil which was low in B, variation in B concentration alone accounted for 28% of the variation in seed yield in spite of 2 kg B/ha having been applied. Marked differences were observed in the leaf nutrient concentrations of 40 inbred lines tested.     

不同林龄樟子松人工林针叶-凋落叶-土壤生态化学计量特征

为明确科尔沁沙地引种樟子松人工林生态系统的C、N、P含量及化学计量特征,采用时空互代的方法,在章古台地区选取4种不同林龄(15,25,35,45年)、立地条件基本一致的樟子松人工林作为研究对象,比较针叶-凋落叶-土壤的C、N、P含量及化学计量比的差异,探讨它们随林龄的变化及其相互间的关系。结果表明:(1)C、N、P含量表现为针叶凋落叶土壤,C/N、C/P、N/P表现为凋落叶针叶土壤,且在3个库之间都有显著差异;(2)林龄对针叶-凋落叶-土壤的C、N、P及C/N、C/P有显著影响,均在35年生樟子松林中针叶-凋落叶-土壤的C、N、P含量最高;(3)相较于其他地区,针叶和凋落叶均表现出高C、P和低N的特征,具有较高的C/N、C/P和较低的N/P;(4)各林龄针叶N/P均小于14,表明该地区樟子松林整个生长过程始终受N的限制,但不同林龄间差异不显著;(5)针叶-凋落叶-土壤的C、N、P含量及其C/N、N/P之间存在显著的相关性,说明该樟子松林生态系统的C、N、P元素在针叶、凋落叶和土壤3个库之间存在运输转换,但其内在维持机制需要进一步深入研究。     

An Investigation on Nutritional Problems of Hazelnut Grown on Acid Soils

Abstract

The purpose of the study was to determine the nutritional problems of hazelnut (Corylus avellana L.) grown on acid soils. For this purpose, soil and leaf samples were taken from 30 different hazelnut growing areas from Trabzon Region in Turkey. Some physical and chemical properties and some nutrient element contents of soil and leaf samples were determined. These determined values were compared with critical values, and the degree of sufficiency was evaluated. In general, organic matter, total nitrogen (N), available phosphorus (P), exchangeable potassium (K), and magnesium (Mg) contents of soil samples were sufficient. Calcium (Ca) deficiency was obtained in 93.4% of the soil, because of acid property of the soils. Available iron (Fe), copper (Cu), and manganese (Mn) contents of the soils were found to be sufficient. In 70% of the soils, Zn deficiency was found. Nitrogen, P, K, Ca, Mg, and Zn deficiencies of leaf samples were 20.0, 26.7, 6.7, 73.4, 50.0, and 66.7%, respectively. Iron, Cu, and Mn contents of leaf samples were found to be sufficient.     

Nutrient mobilization and yield of soybean genotypes

Abstract

Mobilization of nitrogen, phosphorus, and potassium from leaf and carpel tissue during seed growth was estimated for 18 diverse, field‐grown soybean lines and cultivars during two years. The objective was to determine whether lines differed in nutrient mobilization and, if so, whether such differences were related to yielding ability.

Lines differed in nutrient concentration and tissue mass and in nutrient content, both at beginning of seed growth and at plant maturity. Mobilization from leaves and carpels potentially supplied up to 47, 23, and 29% of seed N, P, and K. Leaves were three to four times more important than carpels as sources of seed N and K and nearly twice as important as sources of P.

Only mobilized leaf N exhibited a relationship with seed yield (r = 0.73^?? in 1978 and 0.43^? in 1979). Leaf N mobilization was not heritable (correlation between years for line means was 0.09) in our environment, but might be more so under N‐stress conditions. The major determinant of mobilizable N was leaf mass at beginning of seed growth.     

Soil nutrient supply and biomass production in a mixed forest on a skeleton‐rich soil and an adjacent beech forest

In the natural forest communities of Central Europe, beech (Fagus sylvatica L.) predominates in the tree layer over a wide range of soil conditions. An exception with respect to the dominance of beech are skeleton‐rich soils such as screes where up to 10 broad‐leaved trees co‐exist. In such a Tilia‐Fagus‐Fraxinus‐Acer‐Ulmus forest and an adjacent mono‐specific beech forest we compared (1) soil nutrient pools and net nitrogen mineralization rates, (2) leaf nutrient levels, and (3) leaf litter production and stem increment rates in order to evaluate the relationship between soil conditions and tree species composition. In the mixed forest only a small quantity of fine earth was present (35 g l^—1) which was distributed in patches between basalt stones; whereas a significantly higher (P < 0.05) soil quantity (182 g l^—1) was found in the beech forest. In the soil patches of the mixed forest C and N concentrations and also concentrations of exchangeable nutrients (K, Ca, Mg) were significantly higher than in the beech forest. Net N mineralization rates on soil dry weight basis in the mixed forest exceeded those in the beech forest by a factor of 2.6. Due to differences in fine earth and stone contents, the volume related soil K pool and the N mineralization rate were lower in the mixed forest (52 kg N ha^—1 yr^—1, 0—10 cm depth) than in the beech forest (105 kg N ha^—1 yr^—1). The leaf N and K concentrations of the beech trees did not differ significantly between the stands, which suggests that plant nutrition was not impaired. In the mixed forest leaf litter fall (11 %) and the increment rate of stem basal area (52 %) were lower than in the beech forest. Thus, compared with the adjacent beech forest, the mixed forest stand was characterized by a low volume of patchy distributed nutrient‐rich soil, a lower volume related K pool and N mineralization rate, and low rates of stem increment. Together with other factors such as water availability these patterns may contribute to an explanation of the diverse tree species composition on Central European screes.     

Assessment of mineral nutrition of cork oak through foliar analysis

Abstract

The changes in the mineral nutrient content of the leaves of an evergreen species, the cork oak (Quercus suber L.), were investigated to assess the possibilities of a diagnosis of the mineral nutrition of this forest species. A comprehensive pattern of change in the leaf contents of N, P, and Ca was then put forward from the data obtained. Among the time intervals that are most favorable to analyses, the end of the vegetative rest period, in January, was investigated more precisely. The variation coefficients of the leaf contents measured tree by tree were determined for a number of nutrients (N, P, K, Ca, Mg, Fe, Cu, Zn, Mn, B, Al, and Cl). The foliar analyses carried out on 7‐ to 10‐month old leaves in stands submitted to various forest management practices led to the characterization of significant differences in P, Ca and Mn leaf contents in relation to the treatments applied.     

Effects of climate factors and soil properties on soil nutrients and elemental stoichiometry across the Huang–Huai–Hai River Basin,China

Purpose

Soil nutrients, elemental stoichiometry, and their associated environmental control play important roles in nutrient cycling. The objectives of this study were (1) to investigate soil nutrients and elemental stoichiometry, especially potassium and its associative elemental stoichiometry with other nutrients under different land uses in terrestrial ecosystems; (2) to discuss the impacts of climate factors, soil texture, and soil physicochemical properties; and (3) to identify the key factors on soil nutrient levels and elemental stoichiometry.

Materials and methods

Soil data, including pH, bulk density (BD), cation exchange capacity (CEC), volumetric water content (VMC), clay, silt and sand contents, total carbon (TC), nitrogen (TN), phosphorous (TP) and potassium (TK), available nitrogen (AN), phosphorus (AP), potassium (AK), and soil organic matter (SOM) under different land-use types, were collected, and their elemental stoichiometry ratios were calculated. Climate data including temperature, precipitation, relative humidity, wind speed, and evapotranspiration were collected. The least significant difference test and one-way analysis of variance were applied to investigate the variability of soil nutrients and elemental stoichiometry among land-use types; the ordinary least squares method and the general linear model were used to illustrate the correlations between soil nutrients, elemental stoichiometry, and soil properties or climate factors and to identify the key influencing factors.

Results and discussion

Woodlands had the highest SOM, TN, AN, and AK contents, followed by grasslands, croplands, and shrublands, while the TP and TK contents only varied slightly among land-use types. SOM, TN, AN, N/P, and N/K were strongly negatively correlated to soil pH (p <?0.05) and were strongly positively correlated to soil CEC (p <?0.05). For soil texture, only C/N was moderately negatively correlated to silt content but moderately positively correlated to sand content (p <?0.05). For climate factors, SOM, TN, AN, N/P, and N/K were significantly negatively correlated to evapotranspiration and temperature (p <?0.05), and the correlations were usually moderate. Soil pH explained most of the total variation in soil nutrients, and climate factors explained 5.64–28.16% of soil nutrients and elemental stoichiometry (except for AP (0.0%) and TK (68.35%)).

Conclusions

The results suggest that climate factors and soil properties both affect soil nutrients and elemental stoichiometry, and soil properties generally contribute more than climate factors to soil nutrient levels. The findings will help to improve our knowledge of nutrient flux responses to climate change while also assisting in developing management measures related to soil nutrients under conditions of climate change.