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1.
Nutrient status in Pinus radiata sites in the Basque Country (Spain) have been established. Current-year, 1-year-old needles, and soil samples were collected in 7 sites. Needle samples were analyzed for calcium (Ca), magnesium (Mg), potassium (K), phosphorus (P) and nitrogen (N). Soil samples were analyzed for pH (H2O), N, P, Ca, Mg, K and aluminium (Al). The results indicate differences between sites and needles of different ages. In general, nutrient concentrations in needles are sufficient for the nutritive requirements, but some low concentrations of Mg and P found in 1-year-old needles, indicate that some trees may show signs of deficiency in the near future. In turn, N concentrations are, in many cases, higher than those usually found in this species and may originate growth disorders. These concentrations may be related to NO3 ? and NH4 + deposition. Soil nutrients are sufficient for trees requirements, but the levels of K and Mg are low. Soil pH values are not very acid, and the value of the Ca/Al ratio is, in general, near 1. An arrangement of sites and physiographical and nutritional parameters based on correlation and principal component analysis is also presented.  相似文献   

2.
Abstract

The Mehlich 3 (M3) extractant was introduced in 1981 to improve the efficiency of soil testing laboratories by eliminating the need for multiple extractants for P, K, Ca, Mg, Mn, Cu and Zn. The M3 was also intended to be suitable for a wide range of soils, perhaps to serve as a “universal”; soil test extractant. At present, regional soil testing committees throughout the U.S. are investigating the M3 in this regard.

Development of a field calibration data base for a new soil testing extractant is an essential, but expensive and time‐consuming process. An interim measure is the use of conversion equations between new and current extractant(s). These equations allow for use of the new extractant with existing field calibration data. The objectives of this study were (i) to develop conversion equations for the Mehlich 1 (M1) and M3 extractants for Atlantic Coastal Plain soils, and (ii) to determine the influence of soil pH and organic matter content on the relative extractability of P, K, Ca, Mg, Mn and Zn by Ml and M3.

Four hundred soil samples, obtained from field plots and commercial crop samples submitted to the University of Delaware Soil Testing Laboratory were analyzed for P, K, Ca, Mg, Mn, Cu and Zn by M1 and M3. Highly significant correlations between M3 and M1 were found for all nutrients (r=0.92*** to 0.97***) and, except for Cu and Mn, soil pH and OM did not markedly improve the linear regression equations developed for conversion between M3 and M1. Inclusion of OM in a multiple regression equation between M3 and M1 extractable Cu increased R2 from 0.46** to 0.71***; R2 for Mn+(pH+OM) was 0.48***, relative to 0.35*** for extractable Mn alone. Critical values for M3 P, K, Ca, and Mg, based on conversion equations restricted to soils testing less than high with the M1 extractant, were 41, 49, 295 and 45 mg.dm‐3, respectively. For Mn and Zn, at a pH of 6.2, M3 critical values were 9.5 and 0.6 mg.dm‐3, while for Cu, the M3 critical value ranged from 0.5 to 1.1 mgdm‐3 for soil OM of 2 to 8%.  相似文献   

3.
Abstract

Extractants employed for routine soil analysis vary from one laboratory to another. Lack of a universal soil extractant is a serious limitation for interpretation of analytical results from various laboratories on nutritional status of a given soil. This limitation can be overcome by developing functional relationships for concentrations of a given nutrient extractable by various extradants. In this study, extractability of Ca, Mg, P, and K in a wide range of soils (0–15 cm) from citrus groves in Florida representing 21 soil series, with varying cultural operations, were compared using Mehlich 3 (M3), Mehlich 1 (M1), ammonium acetate (NH4AOc), pH = 7.0 (AA), 0.2M ammonium chloride (NH4Cl), and ammonium bicarbonate‐DTPA (AB‐DTPA) extractants. Soil pH (0.01M CaCl2) varied from 3.57 to 7.28. The concentrations of Ca or Mg extractable by M3, M1, AA, and NH4Cl were strongly correlated with soil pH (r2 = 0.381–0.482). Weak but significant correlations were also found between AB‐DTPA extractable Ca or Mg and soil pH (r2 = 0.235–0.278). Soil pH relationships with extractable K were rather weak (r2 = < 0.131) for M1 and NH4Cl but non‐significant for M3, AB‐DTPA, and AA. Concentrations of Ca, Mg, and K extractable by M3 were significantly correlated with those by either M1, AA, or NH4Cl extractants. Mehlich 3‐P was significantly correlated with P extractable by M1 extractant only. Mehlich 3 versus AB‐DTPA relationship was strong for K (r2 = 0.964), weaker for Mg and P (r2 = 0.180–0.319), and non‐significant for Ca. With the increasing emphasis on possible use of M3 as an universal soil extractant, data from this study support the hypothesis that M3 can be adapted as a suitable extractant for routine soil analysis.  相似文献   

4.
黄土区村级农田土壤养分空间变异特征研究   总被引：15，自引：0，他引：15  
本研究选择黄土高原地区陕西省新集村为研究对象。在219hm2耕地上用网格法采集364个表层(0~20 cm)土壤,研究了该村土壤pH,有机质和速效养分(N,P,K,Ca,Mg,S)空间变异性。结果表明:该村98.9%耕地缺N,缺K,缺P比例占11.5%和4.4%。地统计学分析结果表明:土壤有机质、有效N、P、K、Mg、Ca、S具有中等的空间相关性,空间变异程度依次为:OM>P>Ca>K>Mg>N>S,土壤pH的空间相关性很弱。有机质、有效N、S最大相关距离大,达到1853m,pH值最小,为148m,K、Ca、P、Mg最大相关距离分别为717m、720m、1032m和1344m。施肥是导致该村土壤养分空间变异性的主要原因。基于土壤养分状况和空间分布特征,目前仅需要考虑对该村土壤K,P进行分区管理。  相似文献   

5.
Researchers assessed the spatial distribution of soil chemical properties and nutrients at four depths in a clay loam soil cropped to corn and soybean at Freeman farm of Lincoln University. Soil samples were taken at depths of 0–10, 10–20, 20–40, and 40–60 cm in a 4.05-ha field and analyzed for acidity or basicity (pH), cation exchange capacity (CEC), total carbon (TC), organic matter (OM), base saturations on the CEC, ammonium (NH4+), nitrate (NO3?), phosphorus (P), potassium (K), calcium (Ca), sulfur (S), magnesium (Mg), sodium (Na), manganese (Mn), copper (Cu), iron (Fe), and zinc (Zn). Results showed that coefficients of variation (CV) ranged between 5 and 30%, except for TC, NO3?, and Zn, which had greater CVs. Soil chemical properties and nutrients responded to exponential, linear, Gaussian, and spherical variogram models with nugget-to-sill ratios ≤ 1.0 and effective ranges from 4 to 56 m. Fractal analysis showed that CEC in all depths belonged to the 1.99 ≥ D3 ≥ 1.90 group, which suggests great disorder and antipersistence in the spatial structure.  相似文献   

6.
A study was conducted to examine the impact of land use on soil fertility in an Entisol in the Jalpaiguri District of humid subtropical India. The natural forest served as a control against which changes in soil properties were compared. Soil samples were collected from four different depths (0–25, 25–50, 50–75, and 75–100 cm) of soil from four land uses (viz. forest, home garden, arecanut plantation, and agriculture) and examined for pH, organic carbon (OC), electrical conductivity (EC), cation exchange capacity, available nitrogen (N), phosphorus (P), exchangeable calcium (Ca), magnesium (Mg), potassium (K), aluminum (Al), microbial biomass carbon (MBC), microbial biomass nitrogen (MBN) and dehydrogenase activity (DHA). Soil pH (5.7), OC (2.29%), N (386 kg ha?1), and P (22.54 kg ha?1) were greatest in forest soil, followed by soil from arecanut plantation, agriculture, and home garden. The greatest Ca (0.892 cmol kg?1), Mg (0.527 cmol kg?1), and Al (1.86 cmol kg?1) were found in the arecanut plantation, whereas K (0.211 cmol kg?1) was greatest in forest. The greatest content of diethylenetriaminepentaacetic acid–extractable copper, zinc, manganese, and iron (2.25, 1.66, 4.86, and 7.65 ppm, respectively) were found in forest. MBC (558 mg kg?1), MBN (26.67 mg kg?1), and DHA (33.03 μg TPF 24 h?1 g?1) was greatest in forest soil. Soil fertility index varied from 13.13 in arecanut plantation to 18.49 in forest. The soil evaluation factor ranged from 5.32 in agriculture to 6.56 in forest. Pearson's correlation matrix revealed strongly significant positive correlation of soil fertility index and soil evaluation factor with soil properties.  相似文献   

7.
Abstract

A two‐year study was conducted to determine the macromineral status of cattle grazed forages, mostly bahiagrass, and soils in central Florida. Soil and forage samples were collected every month for two years. Month differences (P < 0.01) were observed in all forage macrominerals and in crude protein (CP) for both years. No month effect (P > 0.05) was observed in IVOMD level during year 1. Year effects (P < 0.05) were observed in calcium (Ca), sodium (Na) and CP. Concentrations below the critical level were observed in all macrominerals studied. Higher forage macro‐mineral concentrations were found during spring‐summer months. In general, higher (P < 0.05) soil aluminum (Al), Ca, magnesium (Mg), phosphorus (P), and organic matter (OM) were observed during fall‐winter months, while Na was higher in winter. Soil Ca and Mg were adequate and potassium (K), Na and P were deficient. Year 2 showed higher (P < 0.05) soil macromineral concentrations. Correlation coefficients (r >|0.5|, P < 0.05) were present between forage K and forage CP (r = 0.557) and between forage P and forage CP (r = 0.554). Low correlations were found between soil and forage macrominerals. Percentages of total forage samples with macromineral and CP concentrations below critical levels (in parentheses) and suggestive of deficiency were as follow: in forage, Ca (0.30 ppm), 21%; Mg (0.18 ppm), 34%; K (0.60 ppm), 47%; Na (0.06 ppm), 89%; P (0.25 ppm), 85%; and CP (7%), 18%.  相似文献   

8.
【目的】土壤养分是植物生存的必要条件,探讨山核桃(Carya cathayensis Sarg.)主产区林地土壤肥力因子及其对土壤生产性能的影响,为山核桃的栽植和可持续发展、土壤培肥提供科学依据。【方法】在浙江省山核桃主产区,随机选择58个典型乡镇的山核桃林采集土样,测定了pH、有机质、碱解氮、有效磷、速效钾、有效钙、有效镁、有效铁、有效锰、有效铜、有效锌、有效硼12个肥力因子水平,运用主成分分析和回归分析方法,分析了它们对山核桃生长、感病等级、产量等级的影响以及丰缺临界区间。【结果】主成分分析前5个因素(PC1、PC2、PC3、PC4、PC5)的累计贡献率达78.49%。PC1的主要荷载为土壤pH、有效钙和有效镁含量,PC2的主要荷载是微量元素和有效磷含量,PC3是有机质和碱解氮含量,PC4和PC5分别是有效硼和速效钾含量。林分生长性状中,生长势等级与pH、速效钾、有效钙、有效镁、有效铜、有效锌显著负相关(P <0.01),干腐病感病等级与pH、有效钙、有效镁显著负相关(P <0.01),产量等级与pH、有效钙、有效镁、有效磷、有效锌显著正相关(P <0.01)。回归模型分析得出,土壤pH、速效钾和有效钙、有效镁、有效铜、有效锌是当前栽培措施水平下影响山核桃生长的关键土壤肥力因子。综合评价后发现,研究区现有约57%的山核桃林地土壤综合肥力低于平均水平。【结论】对山核桃林地土壤生产性能影响最大的因素是土壤pH、有效钙和有效镁含量,其次是微量元素和有效磷含量,有机质、速效钾含量也有一定的影响。山核桃主产区的林地土壤关键指标丰缺范围:pH 5.19~5.70、速效钾87~129 mg/kg、有效钙817~1374 mg/kg、有效镁93~145 mg/kg、有效铜1.36~4.39 mg/kg、有效锌0.78~2.33 mg/kg。  相似文献   

9.
A survey was conducted for assessment of soil fertility status, leaf nutrient concentration and finding yield-limiting nutrients of oil palm (Elaeis guineensis Jacq.) plantations in Mizoram state situated in the northeastern part of India. Soil pH, electrical conductivity (EC), organic carbon (OC), available potassium (K), available phosphorus (P) (Bray's-P), exchangeable calcium (Ca) (Exch. Ca) and magnesium (Mg) (Exch. Mg), available sulfur (S) (CaCl2-S), and hot-water-soluble boron (B) (HWB) content in surface (0–20 cm depth) and subsurface (20–40 cm depth) soil layers varied widely. Diagnosis and Recommendation Integrated System (DRIS) norms were established for different nutrient expressions, and DRIS indices were computed. As per DRIS indices, the order of requirement of nutrients was found to be B > K > Mg > P > nitrogen (N). Optimum leaf nutrient ranges as per DRIS norms varied from 1.91% to 2.95%, 0.46% to 0.65%, 0.63% to 1.00%, 0.48% to 0.88%, and 9.41 to 31.0 mg kg?1 for N, P, K, Mg, and B, respectively. On the basis of DRIS-derived optimum ranges, 32%, 9%, 27%, 12%, and 12% leaf samples had less than optimum concentration of N, P, K, Mg, and B, respectively. The optimum ranges developed could be used as a guide for routine diagnostic and advisory purpose for efficient fertilizer application.  相似文献   

10.
Abstract

Plant samples were taken in an 82.5 ft grid at an early and late sampling date in both 1991 and 1992 from a forty acre field in Illinois. Calcium (Ca) and magnesium (Mg) were analyzed on each sample and maps were made showing the levels of each nutrient within the field. Soil pH measurements were also made from each of the same sampling locations following each year of plant sampling. In the fall of 1991, a calcitic lime application was made using soil pH informations from the 1991 soil sampling to determine the boundaries and rate of the application. Calcium and Mg levels in 1991 roughly defined the area of low pH, except for the early sampled Mg levels. However, low Ca and Mg levels did not always indicate low pH levels. High Ca and Mg levels did not always indicate high pH levels. Following liming, plant Ca levels correlated better with soil pH and represented areas of high and low pH better than plant Mg. Other factors which influenced Ca and Mg levels may have been high levels of competitive cations, disease injured plants, and subsoil pH not described by surface pH measurement.  相似文献   

11.
【目的】明确贵州烟田土壤pH、交换性钙(Ca2+)、交换性镁(Mg2+)和碳酸钙(CaCO3)的含量分布特征及其相互关系,指导土壤酸碱调节及钙镁肥料施用。【方法】采集贵州全省烟区500个典型烟田耕层(0～20 cm)土样,采用经典方法测定土壤p H、Ca2+、Mg2+和CaCO3含量,利用SPSS比较不同成土母质、土壤类型和区域之间pH、Ca2+、Mg2+和CaCO3的含量差异,定量分析pH与Ca2+、Mg2+和CaCO3之间的关系。【结果】土壤pH、Ca2+和Mg2+含量偏低的烟田分别占20.0%、18.2%和56.4%,偏高的烟田分别占37.0%、55.8%和29.6%。CaCO3低于10 g kg-1 烟田占88.4%。不同成土母质、...  相似文献   

12.
Oil palm (Elaeis guineensis Jacq.) is a heavy feeder of nutrients and requires balanced and adequate supply of nutrients for optimum growth and yield. Information regarding soil nutrient status and leaf nutrient concentration is very much required for proper fertilizer application. Therefore, a survey was conducted for assessment of soil nutrient status and leaf nutrient concentration in 64 oil palm plantations in the state of Goa lying in the west coastal region of India. Soil pH, electrical conductivity (EC), organic carbon (OC), available potassium (K) (ammonium acetate-extractable K) (NH4OAc-K), available phosphorus (P) (Bray’s-P), exchangeable calcium (Ca) (Exch. Ca) and magnesium (Mg) (Exch. Mg), available sulphur (S) (calcium chloride-extractable S) (CaCl2-S), and hot water soluble boron (B) (HWB) in surface (0–20 cm depth) soil layers ranged from 4.25 to 6.77, 0.05 to 1.06 dS m–1, 5.07 to 48.4 g kg–1, 58.1 to 1167 mg kg–1, 1.80 to 415 mg kg–1, 200 to 2997 mg kg–1, 36.0 to 744 mg kg–1, 3.00 to 87.7 mg kg–1 and 0.09 to 2.10 mg kg–1, respectively. Diagnosis and Recommendation Integrated System (DRIS) norms were established for different nutrient expressions and were used to compute DRIS indices. As per DRIS indices, the order of requirement of nutrients in the region was found to be P > Mg > K > nitrogen (N) > B. Optimum leaf nutrient ranges as per DRIS norms varied from 1.64 to 2.79%, 0.36 to 0.52%, 0.37 to 0.75%, 0.89 to 1.97%, 0.35 to 0.63%, 0.89 to 1.50%, 3.10 to 13.9 mg kg?1, 7.50 to 32.2 mg kg?1, 35.0 to 91.1 mg kg?1, 206 to 948 mg kg?1, and 895 to 2075 mg kg?1 for N, P, K, Ca, Mg, S, B, copper (Cu), zinc (Zn), manganese (Mn), and iron (Fe) respectively. On the basis of DRIS-derived sufficiency ranges, 14, 5, 11, 6, 6, 6, 8, 2, 3, 6, and 16% of leaf samples had less than optimum concentrations of N, P, K, Ca, Mg, S, B, Cu, Zn, Mn, and Fe respectively. The optimum ranges developed can be used as a guide for routine diagnostic and advisory purpose for balanced utilization of fertilizers.  相似文献   

13.
利用GPS定位采集云南曲靖核心烟田耕层土壤样品651个,测定土样交换性钙、镁及pH、有机质、全氮、全磷、全钾含量,研究交换性钙、镁分布特征及其与土壤其他属性的关系。结果表明:①交换性钙、镁含量均值分别为3 054.3、258.12 mg/kg,变异幅度较大,且两者含量属适宜的占比较低,仅为6.3%和29.8%,总体含量丰富。不同烟区间交换性钙、镁含量差异较大;②交换性钙、镁含量与pH及有机质、全氮、全磷含量呈极显著正相关,交换性钙含量与全钾含量相关性不显著,交换性镁含量与全钾含量呈极显著正相关。采用曲线估计分析每两个属性之间的回归关系,共建立9个拟合曲线函数方程,决定系数为0.118～0.285,拟合误差均在3%以内,拟合优度较好,调节土壤pH、有机质、全氮、全磷和全钾含量对钙镁养分的平衡有重要影响。  相似文献   

14.
Abstract

Few soil test and plant tissue calibration data exist for cucumbers (Cucumis sativus L.). Two years of a singly‐replicated cucumber fertility study were conducted to develop soil and plant data for calibration purposes employing the Boundary Line Approach. Fertility treatments consisting of 4 K levels (as KC1), 3 Mg levels (as MgCl2), 3 pH levels (as Calcitic limestone), and 4 N rates (as urea ammonium nitrate) were factorilly arranged and completely randomized to give 108 treatments in both 1987 and 1988. Analyses were performed upon leaf samples for N, P, K, Ca and Mg at early bloom and soil samples for Mehlich (M) 1‐ and 3‐ P, K, Ca and Mg, and pH. Cucumber yields were determined on early (two fruit pickings) and total (four fruit pickings) sampling periods. High‐yielding cucumbers were attained at soil K (Ml = 64 mg/kg) and Mg (Ml = 29 mg/kg) levels lower than currently recommended. No significant differences in correlation coefficients between either Mehlich (Ml, M3) extractant and cucumber leaf P, K, Ca and Mg concentrations were found. Co‐efficients of determination (R2) values for the relationships (in 1987, 1988) between Ml‐ and M3‐extractable P (0.53, 0.40), K (0.77, 0.64), Ca (0.81, 0.71) and Mg (0.89, 0.74) were all highly significant (P ≤ 0.01). No significant differences were noted between early and total high‐yielding cucumber leaf concentrations and ratios developed for use as preliminary sufficiency ranges and DRIS norms, respectively. A reevaluation of cucumber coastal plain soil test calibrations, especially with regard to K, appears necessary. This study provides further support for the conversion of Ml to M3 soil extraction methodology.  相似文献   

15.
Phosphorus (P) deficiency is one of the most yield-limiting factors in lowland rice production on Brazilian Inceptisol. The objective of this study was to evaluate eight P sources for lowland rice production. The P sources were simple superphosphate (SSP), polymer-coated simple superphosphate (PSSP), ammoniated simple superphosphate (ASSP), polymer-coated ammoniated simple superphosphate (PASSP), triple superphosphate (TSP), polymer-coated triple superphosphate (PTSP), monoammonium phosphate (MAP), and polymer-coated monoammonium phosphate (PMAP). These P sources were applied in four rates (i.e., 50, 100 200, and 400 mg P kg?1) + one control treatment (0 mg P kg?1). Plant height, straw yield, grain yield, panicle number, and root dry weight were significantly increased in a quadratic fashion with increasing P levels from 0 to 400 mg kg?1 of all the P sources evaluated. However, overall maximum root length and P-use efficiency were significantly less at greater P levels. Based on regression equation, maximum plant height was obtained with 262 mg P kg, maximum straw yield was obtained with 263 mg P kg?1, maximum grain yield was obtained with 273 mg P kg?1, and maximum panicle density was obtained with 273 mg P kg?1. Plant growth and yield components had significant positive association with grain yield, except maximum root length. Based on grain yield and average P rate of maximum grain yield, which is 273 mg kg?1, P sources were classified for P-use efficiency in the order of PSSP = TSP > PTSP > PASSP > SSP > MAP > ASSP. Soil chemical properties [pH; P; potassium (K); calcium (Ca); magnesium (Mg); hydrogen (H) + aluminum (Al); cation exchange capacity (CEC); base saturation; Ca, Mg, and K saturation; acidity saturation; Ca/Mg, Ca/K, and Mg/K ratios] changed significantly with the addition of different P treatments.  相似文献   

16.
菜地土壤养分的空间变异特征   总被引：4，自引：2，他引：4  
通过地统计学、空间分析方法及结合农户施肥调查,对菜地土壤养分的空间变异特征进行研究。结果表明,农户施肥水平差别较大,整体上施磷相对过多,施钾相对较少,土壤OM、NH4+-N、P、K、Ca、Mg和S的变异系数在28.4%～69.2%之间。土壤各养分的空间变异结构有较大区别,土壤OM及NH4+-N的变异具有强烈空间相关性,土壤P、K、Ca、Mg和S养分含量的变异为中等空间相关性。土壤养分的等值线图显示,OM在空间的分布与土壤质地渐变规律相关,NH4+-N呈现南北向的带状分布,P、K、Ca、Mg和S趋于小块状分布。总的来说,施肥等人为因素加剧了土壤矿质养分的空间变异。  相似文献   

17.
Soil nutrient deficiencies can affect rice yield and grain mineral content wherever they occur, but an understanding of their effect on upland rice production in humid forest zone of West Africa is still limited. Therefore, a nutrient omission trial was conducted on foot slope soil in 2003, 2004 and 2005 in Côte d’Ivoire using rice variety WAB 56–104. The effect on rice grain yield (GY) and nutrient content of complete fertilizer (Fc with nitrogen (N), phosphorus (P), potassium (K), calcium (Ca), magnesium (Mg) and zinc (Zn)) was compared with Fc from which a specific nutrient was excluded (Fc – N, Fc – P, Fc – K, Fc – Ca, Fc – Mg and Fc – Zn). Before the trial, soil K (0.10 cmol kg?1) and Mg (0.20 cmol kg?1) contents were suitable, but available P-Bray I (4.2 mg kg?1) was found to be deficient. In course of the study, K, Mg and P deficiencies were observed. An antagonistic effect was observed between rice GY and grain concentrations in P, Mg and Ca for treatments Fc – Mg, Fc – P and Fc – K, respectively. Therefore, the use of P, K and Mg fertilizers is recommended for successive cropping seasons in order to rich stable and high rice yield while decreasing of grain concentrations in P, Mg and Ca can be observed.  相似文献   

18.
Abstract

In order to determine the level of horizontal variability, identify its nature in terms of patterns, and propose fertilizer recommendations using coefficient of variability as a factor; eight fields were selected and divided into small units at the MEY Research Station in deep loess hill soils of Northwest Missouri. The size of each unit ranged between 37 to 744 square meters and the size of the field ranged between 0.3 to 1.8 ha. A composite soil sample was collected from each unit and analyzed for extractable P, K, Ca, Mg, organic matter (OM) content, and salt pH. The coefficient of variation of each test in each field was computed.

The data indicated that the weighted mean of the coefficient of variation of the whole experimental area (6.1 hectares) for pH, P, K, Ca, Mg, and OM was 5, 43, 35, 16, 24, and 54 percent, respectively. There appeared to be some low and high points in soil test levels of each field, but the patterns were not large enough to justify variable fertilizer application or economically valid for collecting and analyzing separate samples.

Based on this data, it appears that the fields showing optimum levels of ? and ? might have 50% of the area below optimum. To optimize the yield potential of the whole field, there should be a two step approach in fertilizer recommendations. The first step should be to build ? and ? to conventional optimum levels. Once the conventional optimum levels are achieved, the second step should be to build to even higher levels of ? and K, the basis being established by a coefficient of variability factor.  相似文献   

19.
Association between lowland grassland plant communities and soil properties   总被引：1，自引：0，他引：1  
Soil properties should be taken into account when managing and restoring semi-natural grasslands. Topsoils sampled at 462 sites in temperate lowland grasslands in England, UK, were analysed for pH, extractable phosphorus (P), potassium (K) and magnesium (Mg), total nitrogen (N), organic matter (OM), and estimated available water capacity. Soil-plant community relationships were determined using Canonical Correspondence Analysis. Mesotrophic semi-improved grasslands had soil nutrient levels closer to semi-natural communities than to agriculturally improved grasslands, and will be suitable targets for restoration. Unimproved mesotrophic sub-communities were distributed along a pH gradient and will be sensitive to soil pH changes. Wet grasslands were differentiated at the community level; the most species-rich had low extractable P and K levels and will require high levels of soil wetness. Calcareous grasslands were less well differentiated from one another but had lowest ecological amplitudes. Soil summary data for communities are presented to assist site managers and policy makers.  相似文献   

20.
Abstract

Selected chemical properties of an artificially acidified agricultural soil from northern Idaho were evaluated in a laboratory study. Elemental S and Ca(OH)2were used to manipulate the soil pH of a Latahco silt loam (fine‐silty, mixed, frigid Argiaquic Xeric Argialboll), which had an initial pH of 5.7. A 100 day incubation period resulted in a soil pH manipulation range of 3.3 to 7.0. Chemical properties evaluated included: N mineralization rate, extractable P, AI, Mn, Ca, Mg and K and CEC. N mineralization rate (assessed by anaerobic incubation) decreased with decreasing soil pH. Nitrification rate also decreased as NH4 +‐N accumulated under acid soil conditions. Sodium acetate extractable P was positively linearly correlated (R2= 0.87) with soil pH over the entire pH range evaluated. Potassium chloride extractable Al was less than 1.3 mg kg‐1of soil at pH values higher than 4.4. Consequently, potential Al toxicity problems in these soils are minimal. Extractable Mn increased with decreasing soil pH. Soil CEC, extractable Mg, and extractable K all decreased with increasing soil pH from 3.3 to 7.0. Extractable Ca levels were largely unaffected by changing soil pH. It is likely that the availability of N and P would be the most adversely affected parameters by soil acidification  相似文献   

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