Tree encroachment into savannas alters soil microbiological and chemical properties facilitating forest expansion

Forests have been expanding over typical savanna sites for the past 3000 years in the Neotropics.Such invasion can produce a series of environmental modifications on typical savanna;however,it remains unclear how modifications in soil properties,caused by the encroachment of woody species,facilitate the expansion of forest ecosystems under dystrophic conditions.Here we examined chemical and microbiological changes associated with tree encroachment in oxisols of a Neotropical Savanna at Assis Ecological Station,Southeastern Brazil.We predicted that tree encroachment caused by typical forest species would cause significant changes in the chemical and microbiological properties of savanna soils.Soils were sampled at Assis Ecological Station,from savanna sites differing in tree encroachment(typical,dense and forested savanna) caused by decades of fire exclusion.We analysed vegetation leaf area index and leaf litter volume deposited in the studied plots and chemical(pH,organic matter,P,K,Ca,Mg,Al,NO_3~-,NH_4~+) and microbiological(microbial C biomass and dehydrogenase activity) properties of soils under distinct encroachment conditions.Most soil chemical properties did not change along the tree encroachment gradient;however,total P,soil organic matter,soil microbial C and dehydrogenase activity increased from typical savanna to forested savanna.The changes in soil organic matter and dehydrogenase activity were correlated with the values of leaf area index and litter volume along the encroachment gradient.Our results demonstrate that forest species can increase carbon and phosphorus supplies in tropical savanna soils.     

Change in soil macrofauna and vegetation when fast-growing trees are planted on savanna soils

Many forest species can be found in understory vegetation of old plantation plots, despite the fact that the native vegetation was a poor savanna growing on highly nonfertile sandy soils. The aim of the present paper is to describe the changes that occur in the environmental conditions when savanna is planted with fast-growing trees, and is particularly concerned with vegetation and soil macrofauna. The study was carried out in industrial eucalyptus plantations, and in experimental Acacia and pine plantations. Most plots were located on sandy soil, but some measurements were also carried out on clay soil planted with the same species in order to assess the influence of soil type.

A strong correlation was shown between the age of the eucalyptus trees and the percentage of forest species in undergrowth, emphasizing the progressive change from savanna vegetation towards forest vegetation.

Biomass and density of macrofauna were very low in both sandy and clayey savanna soils, total biomass being 3.3 and 5.8 g/m² respectively. Soil macrofauna became more important as the age of plantations increased, and biomass reached 29 g/m² in the 20-year-old eucalyptus plot on sandy soil, and 74 g/m² in 26-year-old eucalyptus plantation on clay soil, compared to 33 g/m² in the natural forest plot on sandy soil; however, frequency of occurrence and number of taxa were lower in old eucalyptus plot as compared to forest. Large differences in the abundance of macrofauna were observed in relation to planted species. Acacia was most favourable to soil macrofauna, with a total biomass of 60 g/m² on sandy soil and many taxa present. Pine plantations had a poor macrofauna and several taxa were lacking, particularly in the sandy soil.

Total macrofauna frequency was significantly correlated with the percentage of forest species in understory vegetation. Both were correlated with soil pH and soil organic-matter content. The results suggest that soil organic matter and litter quality are of main importance in changing the above- and below-ground habitat in plantations.     

湘东大围山垂直带表层土壤肥力质量分析

为了解山地土壤肥力质量的垂直地带性分异规律,选取中亚热带典型花岗岩中山(湘东大围山)土壤垂直带,沿海拔梯度采集21个调查样地的表层土壤样品,室内分析14项土壤物理、化学指标(砂粒含量、粉粒含量、黏粒含量、容重、pH值、有机质含量、全氮含量、全磷含量、全钾含量、碱解氮含量、有效磷含量、速效钾含量、阳离子交换量和盐基饱和度),基于主成分分析法构建土壤肥力质量评价的最小数据集,探索土壤肥力质量指数、土壤理化性质与海拔的关系。结果表明,土壤肥力质量评价最小数据集包括黏粒含量、阳离子交换量、有机质含量、有效磷含量和速效钾含量5项指标。土壤有机质、全氮含量和阳离子交换量均随海拔升高呈先减少后增加的趋势,土壤全磷和有效磷含量与海拔呈显著正相关。土壤类型(亚类)也显著影响土壤有机质、有效磷含量和阳离子交换量,均以灌丛草甸土最多,红壤最少。土壤肥力质量综合指数随海拔升高呈先降低后升高的趋势,按指数大小由高到低划分为4个等级,52%的调查样地处于中等偏上水平。中亚热带大围山花岗岩中山土壤肥力质量总体中等偏上,土壤肥力质量指数具有明显的高度带现象,山地土壤保育与开发中应重视土壤质量的垂直地带性分异规律。     

Soil factors influencing yields of Eucalyptus camaldulensis on former tin-mining land in the Jos Plateau region,Nigeria

Plantations of Eucalyptus growing on reclaimed tin-minning spoil were compared with similar stands established on undisturbed farmland soils in the north of the Jos Plateau, Nigeria. Soils were collected from sample plots in both situations to determine their physical and chemical properties, while destructive harvests of representative stems were used to calculate tree yields.A principal components analysis of the soils data revealed wide variations in texture and base status, and was supported by a cluster analysis from which five major soil groups were defined. One such group, which contained a majority of mining site plots, was characterised by shortages of organic matter and low levels of available phosphorus. Farmland plantation sites had a wider range of texture and fertility, but on the whole gave similar yields to those of mining sites.The relationship between forest yield and selected soil variables was investigated using multiple regression analysis. This showed that the best yields occurred on fine-textured soils with good reserves of organic matter, while moderately base-saturated soils and high available-iron concentrations were associated with poor growth. There were indications that soil chemistry was modified by tree growth, with high-yielding stands increasing cation exchange capacity but significantly lowering soil pH.The implications for future tree growth are discussed, and suggestions given for the improvement of currently derelict mining sites.     

Tree-grass relationships in open eucalypt woodlands of northeastern Australia: influence of trees on pasture productivity, forage quality and species distribution

Pasture yield, quality and species distributions were compared between zones around live and killed eucalypt trees at two woodland sites in northeast Queensland which differed markedly in soil fertility. Trees affected pasture quality and yield on an individual tree basis: N concentration and dry matter digestibility tended to be higher under trees than in inter-tree areas at both sites and pasture yields declined with distance from killed trees at the lower fertility site. However, the distribution of individual species did not vary markedly with distance from trees. Trees also affected pasture yield on a woodland basis: yields were greater where the trees were killed than under intact woodland. Soil under trees had higher levels of organic carbon and greater litter cover than soil in inter-tree areas. However, pasture yields did not generally reflect this fertility gradient since growth was limited by moisture availability due to drought conditions during the study period. Pasture N concentration was higher under trees that in inter-tree areas since plants under trees produced a similar amount of biomass as plants in inter-tree areas, but had access to higher nutrient levels. Trees appeared to have a greater effect on soil nutrient availability at the low fertility site. Live trees depressed pasture yields to a lesser degree at the low fertility site, demonstrating that the effects of trees on soil water availability (on a woodland scale) are less important when soil nutrients are more limiting to growth. These results indicate that, while removing trees may enhance pasture productivity, this benefit may be offset by a reduction in pasture quality. Given the beneficial effect of trees on soil nutrients, tree removal may also have longer term implications for soil nutrient dynamics. This revised version was published online in August 2006 with corrections to the Cover Date.     

Millettia ferruginea from southern Ethiopia: Impacts on soil fertility and growth of maize

Growing agricultural crops under Millettia ferruginea (Hochst.) Baker, a tree that is endemic to Ethiopia, is an age-old practice in the country, but the beneficial effects of the tree on crops have not been scientifically quantified. To achieve this, four isolated and nearly identical Millettia trees growing on similar site conditions were selected and canopy coverage of each tree was divided into four radial transects. Four plots of 0.5 × 0.5 m were established on each radial transect at 0.5 to 1, 2.5 to 3, 4.5 to 5, and 6.5 to 7 m away from the tree bases. The control plot was established at 29.5 to 30 m. Composite soil samples from each of the four plots located at a comparable distance and at two soil depths, 0 to 10 and 20 to 30 cm, were collected and analyzed. The level of surface soil P, organic C, exchangeable base-forming cations and cation exchange capacity were all significantly higher (P < 0.000 to P < 0.015) under the trees than in the open field. Nutrient levels declined with depth and increasing distances from the tree trunk. Soil pH values did not show significant horizontal or vertical variations in all the soil samples analyzed. Maize plants grown on soils collected from underneath Millettia trees resulted in significantly better growth responses and higher dry matter yield as compared to the control (P < 0.001). Socioeconomic studies indicated that Millettia trees have good standing in the region both because of their desirable biological characteristics and because of their economic benefits.This revised version was published online in November 2005 with corrections to the Cover Date.     

广州市绿地土壤质量评价及其管理对策

对广州市各类绿地土壤调查表明,绿地土壤质地主要为砂质粘壤土和粘壤土;pH值多为中性至碱性;有机质、全氨、水解氨、速效钾含量偏低;土壤的全磷缺乏,速效磷、全钾含量中等;土壤容重大;绿地土壤综合肥力一般甚至贫瘠。综合分析了广州绿地土壤质量,提出具体管理对策。     

Soil amelioration and root symbioses ofParkia biglobosa (Jacq.) Benth. in West Africa

Parkia biglobosa is an important multipurpose tree from the savanna zone of West Africa. It has been reported to increase soil fertility and crop yields beneath its crown. However, no work has been conducted to determine the role of root symbioses in soil amelioration by this species. The existing reports of nodulation inParkia biglobosa are contradictory and the presence of mycorrhizae is not documented in the literature.Fieldwork was conducted at six sites in Burkina Faso and Nigeria, to investigate the amelioratory effect ofParkia biglobosa on soil fertility and to ascertain the occurence of root symbioses. Soil samples were collected from points close to the trunk, the mid-crown, crown edge and the open areas away from individual trees. The samples were analysed chemically to assess pH, organic matter, nitrogen, phosphorus and potassium content. Root samples were also collected from the field and examined for nodules and for evidence of mycorrhizal infection.The results of the soil analysis showed a significant amelioration for total nitrogen and available potassium with proximity to the tree, but organic matter, available phosphorus and soil pH showed no significant trend. This pattern was similar for all sites. The results also indicated that amelioration of nitrogen and potassium with proximity to the tree increased with tree size.Root nodules were absent from the roots of trees examined in the field, both in Burkina Faso and Nigeria. A pot experiment was set up using the soil collected from beneath the trees and a laboratory grown cowpea miscellany culture as rhizobial inoculum forParkia biglobosa seedlings. The roots of these seedlings also showed no evidence of nodulation. Ectomycorrhizae were not present in roots collected from the field, but endomycorrhizal infection was prolific.A study of root distribution in Burkina Faso suggested that one mechanism for increased soil fertility beneathParkia biglobosa is the widespread lateral root system, which redistributes nutrients from an extensive radius to a concentrated area beneath the crown. The root system is aided in the efficient uptake of nutrients by endomycorrhizae. Other possible mechanisms include interception of dust by the crown and deposition by throughfall and stemflow, defacation by animals beneath the tree and decomposition of leaf litter.     

广东省桉树林的土壤肥力研究

利用2002年广东省森林资源与生态状况综合监测评估体系的95个桉树林样地的调查资料研究了桉树林的土壤肥力。按《我国土壤质地暂行分类方案》将95个样地土壤合并为粉壤土、粘壤土、粗砂土、细砂土、面砂土、粉粘土、砂粘土、粘土、壤粘土。通过对土壤理化性质进行聚类分析,将土壤按质地类型划分为4类：第1类包括粉壤土、粉粘土和壤粘土,速效K含量较高,速效P含量中等,其余养分含量位居9种土壤的前列,容重和毛管孔隙中等,肥力较高;第2类是粘壤土,全K含量最高,速效N含量中等,其余养分含量较低,容重较小,毛管孔隙较大而非毛管孔隙中等,总体上肥力水平中等;第3类包括粗砂土、细砂土、面砂土和砂粘土,此类土大多数有机质、全N、全K、速效N、速效K含量低,而有的速效P含量较高,容重大、毛管孔隙小,总体来说肥力低;第4类为肥力高的粘土,其有机质、全N、全P、速效N、速效P含量均是9种土壤中最高的。     

Reclaiming sodic soils for wheat production by Prosopis juliflora (Swartz) DC afforestation in India

A green house pot trial was conducted to assess the impact of Prosopis afforestation on the productivity and fertility of degraded sodic soils in Haryana, India. Wheat (Triticum aestivum, L; cultivar HD 2329) plants were grown from seed on top soils collected from a chronosequence of 0, 5, 7, and 30-year-old Prosopis juliflora plantations established on highly sodic soils and a non-sodic reference soil collected from a local farm. The afforestation improved physical and chemical properties of surface soils by decreasing pH, electrical conductivity and exchangeable Na levels, and increasing infiltration capacity, organic C, total N, available P, and exchangeable Ca, Mg, and, K levels. The amelioration effect of the trees on top soil increased with duration of tree occupancy. Soil nutrient status under the 30-year-old plantation was higher than that of the non-sodic farm soil. The reduced soil sodicity and improved fertility contributed to higher germination, survival, growth, and grain yield of wheat plants grown on the Prosopis chronosequence soils, even surpassing the yield attained on the farm soil in the case of 30-year-old plantation soil. Sodium accumulation in the crop declined while N, P, K, Ca, and Mg uptake increased with soil plantation age reflecting the changing nutrient status of the rooting zone due to afforestation. Results confirmed that successful tree plantation may restore the productivity and fertility of highly degraded sodic soils.     

不同施肥对雷州半岛桉树林地土壤培肥效应研究

本文研究了雷州半岛两种主要类型砖红壤有机肥与无机肥配施对桉树土壤养分特征和土壤培肥效应。结果表明:在雷州半岛低地力的土壤中种植桉树时,浅海沉积物发育的砖红壤有机质有所提高,而玄武岩砖红壤有机质下降;土壤有机质含量与林木生长量相关性为极显著水平,与施肥量的相关性较低,未达到显著水平。随施有机肥数量的增加,有机质呈上升趋势。施用滤泥1.5～2.5 kg.株-1时,土壤有机质比单施无机肥提高0.02%～0.21%,比不施肥提高0.07%～0.26%。经施肥后5a测定,施有机肥处理容重比施无机肥的降低0.01%～0.22%,总孔隙度比施无机肥的提高0.1%～7.1%,说明施用有机肥改良砖红壤物理特性。因此,两种类型砖红壤中有机肥施用对桉树土壤肥力具有极显著培肥效应。     

Islands of fertility: Soil improvement under indigenous homegardens in the savannas of Roraima,Brazil

Homegardens are a common feature of indigenous dwellings in the savannas of Roraima, northern Brazil. In order to evaluate the effect of homegardens on soils, samples were taken in 5 sites each in the categories new homegardens (0–10-years old), established homegardens (15–35-years old) and old homegardens (more than 40-years old) and in adjacent savanna in Araçá Indigenous Land, Roraima, Brazil. For comparison, samples were also taken in forest islands located nearby, on a different soil type, under 10-year-old forest fallows and high forest. P and K showed the greatest increases over time in homegarden soils, in comparison with levels found in adjacent savanna and under forest. Ca and Mg also increased in comparison to adjacent savanna, but levels were less than found in forest soils, most likely due to the different parent material. Zn and Fe also showed increases in homegarden soils over time. Cu and Mn levels showed little relation to homegarden age, suggesting greater effects of factors of soil formation than anthropogenic influences. Values for pH were slightly higher in homegardens than in adjacent savanna, while Al was lower, although these changes were poorly fit by regression models. Soil organic matter increased over time under homegardens, but still was lower than levels found under fallows and forest. Soil fertility improvement under indigenous homegardens can be attributed mainly to deposition of residues around dwellings, although further investigation is needed on the role of trees in accessing nutrient pools at greater depths in savanna soils.     

Charge characteristics of soil organic matter fractions in a Ferric Lixisol under some multipurpose trees

Soil organic matter (SOM) has a key role in maintaining soil fertility in weathered soils in the tropics. This study was conducted to determine the contribution of different SOM fractions to the cation exchange capacity (CEC) of a tropical soil as influenced by organic matter inputs of different biochemical composition. Soil samples were collected from a 16-yr old arboretum established on a Ferric Lixisol, under five multipurpose tree species: Leucaena leucocephala, Dactyladenia barteri, Afzelia africana, Pterocarpus santalinoides, and Treculia africana. Fractions were obtained by wet sieving and sedimentation after dispersion with Na₂CO₃. Fractions larger than 0.053 mm were separated into mineral and organic components by flotation on water. Relationships between CEC and pH were determined using the silverthioureum-method. For all treatments the organic fractions had the highest CEC, expressed on a dry matter basis, and the CEC of the fractions smaller than 0.053 mm was inversely related to their particle size: clay (< 0.002 mm) > fine silt (0.002–0.02 mm) > coarse silt (0.02–0.053 mm). A positive correlation (significant at the 0.01 probability level) existed between the slope of the fitted CEC-pH relationships and the organic C concentrations of the whole soil and both silt fractions. The clay and fine silt fractions were responsible for 85 to 90% of the CEC of the soil. Organic inputs with a high C/N and lignin/N ratio produced fine and coarse silt sized SOM fractions with the highest charge density. Therefore, inputs of slowly decomposing organic residues seem to be promising for increasing the CEC of highly weathered soils.This revised version was published online in November 2005 with corrections to the Cover Date.     

Soil organic carbon and aggregation under poplar based agroforestry system in relation to tree age and soil type

The poplar based agroforestry system improves aggregation of soil through huge amounts of organic matter in the form of leaf biomass. The extent of improvement may be affected by the age of the poplar trees and the soil type. The surface and subsurface soil samples from agroforestry and adjoining non-agroforestry sites with different years of poplar plantation (1, 3 and 6 years) and varying soil textures (loamy sand and sandy clay) were analyzed for soil organic carbon, its sequestration and aggregate size distribution. The average soil organic carbon increased from 0.36 in sole crop to 0.66% in agroforestry soils. The increase was higher in loamy sand than sandy clay. The soil organic carbon increased with increase in tree age. The soils under agroforestry had 2.9–4.8 Mg ha⁻¹ higher soil organic carbon than in sole crop. The poplar trees could sequester higher soil organic carbon in 0–30 cm profile during the first year of their plantation (6.07 Mg ha⁻¹ year⁻¹) than the subsequent years (1.95–2.63 Mg ha⁻¹ year⁻¹). The sandy clay could sequester higher carbon (2.85 Mg ha⁻¹ year⁻¹) than in loamy sand (2.32 Mg ha⁻¹ year⁻¹). The mean weight diameter (MWD) of soil aggregates increased by 3.2, 7.3 and 13.3 times in soils with 1, 3 and 6 years plantation, respectively from that in sole crop. The increase in MWD with agroforestry was higher in loamy sand than sandy clay soil. The water stable aggregates (WSA >0.25 mm) increased by 14.4, 32.6 and 56.9 times in soils with 1, 3 and 6 years plantation, respectively, from that in sole crop. The WSA >0.25 mm were 6.02 times higher in loamy sand and 2.2 times in sandy clay than in sole crop soils.     

Effects of soil pH gradient caused by stemflow acidification on soil microarthropod community structure in a Japanese red cedar plantation: An evaluation of ecological risk on decomposition

Effect of acidic stemflow input on soil biological properties around cedar tree trunk were examined in a 34 year old Japanese red cedar plantation forest. Average soil pH of soil around cedar trunk (stemflow soil) was 3.88 and that of soil between trees (throughfall soil) was 4.97, and this suggested soil acidification due to proton load via stemflow. Soil microarthropod density in soil was higher as close to tree trunk, whereas microbial biomass of surface soil was reduced ca. 30 % around trunk. Abundance of Collembola and Gamasid mites showed positive correlation to amount of soil organic matter, while Oribatida had strong negative correlation to soil pH.Tectocepheus velatus (Oribatida) was dominant in soils pH under 4.0. Annual decomposition rate of cedar foliage was reduced ca. 16% in stemflow soil compared to throughfall soil. More litter accumulation was observed in stemflow soil, but it was not significant, though low microbial activity and retarded litter decomposition may be responsible to the accumulation of organic matter in stemflow soil. Soil biological community and soil process have been changed due to stemflow, the affected area corresponded to ca. 9.4 % of the forest. Thus, ecological risk of acidification in the sense of decrease in decomposition rate is 1.4%. This study was partly supported by Grant-in-Aid for Scientific Research (A)(1), No.08506001 by The Ministry of Education, Science, Sports, and Culture, Japan, and by the research project “Establishment of a scientific framework for the management of toxicity of chemicals based on environmental risk-benefit analysis” supported by Core Research for Evolutional Science and Technology (CREST).     

Bioamelioration of a sodic soil by silvopastoral systems in northwestern India

In sodic soils, excessive amounts of salts have an adverse effect on soil biological activity and stability of soil organic matter. The study analyzes the role of silvopastoral systems to improve soil organic matter and microbial activity with a view for effective management of soil fertility. The silvopastoral systems for the present study (located at Saraswati Reserved Forest, Kurukshetra; 29°4′ to 30°15′ N and 75°15′ to 77°16prime; E) are characterized by tree species of Acacia nilotica, Dalbergia sissoo and Prosopis juliflora along with grass species of Desmostachya bipinnata and Sporobolus marginatus. Soil microbial biomass carbon was measured using the fumigation extraction technique and nitrogen mineralization rates using aerobic incubation method. The microbial biomass carbon in the soils of D. bipinnata and S. marginatus treatments were low. In silvopastoral systems, microbial biomass carbon increased due to increase in the carbon content in the soil – plant system. A significant relationship was found between microbial biomass carbon and plant biomass carbon (r = 0.83) as well as the flux of carbon in net primary productivity (r = 0.92). Nitrogen mineralization rates were found greater in silvopastoral systems compared to 'grass-only' system. Soil organic matter was linearly related to microbial biomass carbon, soil N and nitrogen mineralization rates (r = 0.95 to 0.98, p < 0.01). On the basis of improvement in soil organic matter, enlarged soil microbial biomass pool and greater soil N availability in the tree + grass systems, agroforestry could be adopted for improving the fertility of highly sodic soil. This revised version was published online in June 2006 with corrections to the Cover Date.     

昆明市野鸭湖景区的土壤特性研究

通过对昆明市野鸭湖景区不同的植被类型及土壤类型设样调查。其调查研究的结果表明:该景区的主要土壤类型有山地红壤、山地黄红壤、黄壤、黄棕壤、黄色砂壤等5种类型,红壤、黄红壤、黄壤基本各占1/3,土壤质地大多数是粘壤土。主要成土岩石有石灰岩、砂岩、变质岩(板岩、片岩)、红色砂岩、紫色砂岩等,主要成土母质有残积母质、坡积母质等类型;为酸性土壤,土壤的有机质含量较低,缺乏有效氮,严重缺乏有效磷,土壤交换性能较差,肥力偏低,且土壤的侵蚀现象明显。据此,应防止景区植被的进一步破坏。     

Changes in soil properties and vegetation characteristics along a forest-savanna gradient in southern Venezuela

Vegetation cover in the Gran Sabana highlands (southern Venezuela) appears as a complex mosaic of tall to low forests, bush vegetation and savannas. In this study we described the changes in structure and floristic composition along a forest-savanna gradient consisted of tall forest (TF), medium forest (MF), low forest (LF) and open savanna (S), and analyse the possible reasons for the observed changes. The results showed no obvious differences in the soils properties along the vegetation gradient. All sites presented shallow soils (<50 cm depth) with high percentage of sand and with dominance of quartz, kaolinite and oxides of iron and aluminum. The soil chemical characteristics were unfavorable and similar along the vegetation gradient. The major soil difference was related with the presence of an organic layer on the soil surface of TF and MF and their absence on the soils of LF and S. Abundant residues of large trees were found on the forest floor of TF, MF and LF. These residues presented no signs of burning in TF, while in MF and particularly in LF were charred. This observation joined to the presence of charcoal within the mineral soil of S and the absence of the organic surface layer in LF and S indicated that fire has affected with different intensity or frequency the studied vegetation gradient. Large differences in the structure and floristic composition were found between TF, MF, LF and S. These differences could not be explained by changes in the mineralogical and chemical characteristics of the soil but only by fire which triggers the conversion. We concluded that the studied vegetation gradient represents stages in a temporal change from forest to savanna caused by fire, and this change has implied an impoverishment of tree species, a drastic reduction of biomass in terms of basal area, a drastic change of the floristic composition and the loss of the organic surface layer, which play an important role to maintain the fertility of these soils.     

Soil improvement by trees in sub-Saharan Africa

Trees can influence both the supply and availability of nutrients in the soil. Trees increase the supply of nutrients within the rooting zone of crops through (1) input of N by biological N₂ fixation, (2) retrieval of nutrients from below the rooting zone of crops and (3) reduction in nutrient losses from processes such as leaching and erosion. Trees can increase the availability of nutrients through increased release of nutrients from soil organic matter (SOM) and recycled organic residues. Roots of trees frequently extend beyond the rooting depth of crops. Research on a Kandiudalfic Eutrudox in western Kenya showed that fast-growing trees with high N demand (Calliandra calothyrsus, Sesbania sesban and Eucalyptus grandis) took up subsoil nitrate that had accumulated below the rooting depth of annual crops. Sesbania sesban was also more effective than a natural grass fallow in extracting subsoil water, suggesting less leaching loss of nutrients under S. sesban than under natural uncultivated fallows. Nutrient release from SOM is normally more dependent on the portion of the SOM in biologically active fractions than on total quantity of SOM. Trees can increase inorganic soil N, N mineralization and amount of N in light fraction SOM. Among six tree fallows of 2- and 3-year duration on an Ustic Rhodustalf in Zambia, inorganic N and N mineralization were higher for the two tree species with lowest (lignin + polyphenol)-to-N ratio (mean = 11) in leaf litter than for the two tree species with highest ratio (mean = 20) in leaf litter. Trees can also restore soil fauna, which are important for SOM and plant residue decomposition. Some agroforestry trees have potential to provide N in quantities sufficient to support moderate crop yields through (i) N inputs from biological N₂ fixation and retrieval of nitrate from deep soil layers and (ii) cycling of N from plant residues and manures. The cycling of P from organic materials is normally insufficient to meet the P requirements of crops. Sustained crop production with agroforestry on P-deficient soils will typically require external P inputs. This revised version was published online in June 2006 with corrections to the Cover Date.     

Nutrition and growth of wheat–sorghum rotation in soils amended with leaf litter of trees before planting of wheat

Nutrient release from plant residues can be manipulated as per crop demand through several approaches. A pot study was conducted to study the influence of incorporation of leaf litter of poplar (Populus deltoides), eucalypt (Eucalyptus hybrid) and dek (Melia azedarach) inoculated with cellulolytic fungus culture (Aspergillus awamori) on the nutrition and biomass of wheat (Triticum aestivum, cv. PBW 343) in loamy sand and sandy loam soils. The residual effect of leaf litter after wheat harvest was studied on sorghum (Sorghum bicolor, cv. Punjab Sudax Chari 1). The treatments consisted of a control (no leaf litter) and three uninoculated as well as inoculated leaf litter levels of tree species–0.15%, 0.30% and 0.45% (w/w, dry weight basis). A uniform dose of N, P and K @ 50, 11 and 10 mg kg⁻¹ soil, respectively from inorganic fertilizers was applied to all the treated pots. Straw and grain yield, and nutrient content of wheat increased with increasing level of uninoculated or inoculated leaf litter in both the soils. The inoculated leaf litter augmented the yield and nutrient content of crop significantly (P < 0.05) as compared to the corresponding uninoculated treatments. Poplar and dek leaf litter produced higher wheat yield, plant nutrient content and available nutrients in soil after wheat harvest than eucalypt leaf litter. Dry matter yield of sorghum raised on residual fertility increased significantly with increasing levels of leaf litter application. The comparative responses in yield and nutrient content of crops were higher in loamy sand than in the sandy loam soil. The study shows the beneficial influence of use of cellulolytic microorganisms on enhancement in decomposition and nutrient release from litterfall of tree species.