不同土壤水分条件下容重对玉米生长的影响

用玉米作为实验材料。进行分根实验研究不同土壤水分条件下容重对玉米生长的影响,种子根平分在装有塿土的分隔的白铁皮桶中,土壤容重分4种处理：低容重(两边容重都为1．20g·cm^-3)、中容重(两边容重都为1．33g·cm^-3)、高容重(两边容重都为1．45g·cm^-3)和混合容重(一边为1．20g·cm^-3,另一边为1．45g·cm^-3),土壤水分控制在高基质势(-0．17MPa)和低基质势(-0．86MPa)两个水平,结果表明,当植株生长在紧实土壤或土壤基质势从-0．17MPa降到-0．86MPa时。根长、根干重和地上部干重都显著降低,并且地上部干重的降幅更大,紧实土壤使根长降低的同时还使根的直径增大,无论是容重增大还是土壤水分含量降低所引起的高土壤阻力都使叶片扩展速度降低和植株变小,生长在紧实土壤中的植株变小不仅是因为叶片扩展速度降低,同时是成熟叶片叶面积缩小的结果。然而,当植株生长在混合容重土壤中时,处在低容重土壤中的根系生长得到加强,补偿甚至超补偿高容重土壤中根系生长的不足,整个植株的生长状况与低容重土壤中生长的植株接近。     

Rhizosphere carboxylate concentrations of chickpea are affected by soil bulk density

We investigated whether carboxylate exudation by chickpea (Cicer arietinum L.) was affected by soil bulk density and if this effect was local or systemic. We hypothesised that concentrations of carboxylates would increase with distance from the root apex due to continuous and constitutive accumulation of carboxylates, and that exudate accumulation would be greater in a compacted soil than in a loose soil. Plants were grown in split-root or single cylinders containing loose (1400 kg m (-3)) or compacted (1800 kg m (-3)) soil. Rhizosphere carboxylate concentrations were measured of whole root systems as well as of sections along the root. The root diameter was greatest of plants grown in the compacted soil; however, root diameters were the same for both root halves in the split-root design, whether they grew in loose soil or in compacted soil. Similarly, carboxylate concentrations tended to be lower for the whole root system in the compacted soil, but were the same for both root halves in the split-root design, irrespective of whether the roots were in loose soil or in compacted soil. These results indicate that both root diameter and carboxylate exudation by roots in chickpea is regulated systemically via a signal from the shoot rather than by local signals in the roots. There was no accumulation of carboxylates with increasing distance from the apex, probably because microbial degradation occurred at similar rates as carboxylate exudation. Malonate, previously suggested as deterrent to microorganisms, is likely only a selective deterrent.     

The effect of heterogeneous soil bulk density on root growth of field-grown mangrove species

Background and aims

In Australia’s Mediterranean hyperdiverse vegetation, species that produce cluster roots to mobilise poorly-available nutrients (e.g. Banksia spp.) are an important functional and structural component. Cluster roots are only active during the wet season, indicating a strong dependence on suitable surface soil moisture conditions. Winter rainfall in this region is declining due to global climate change, with a delayed commencement of rains and a decline in precipitation. It is unknown how lower soil moisture levels will affect the root dynamics of these globally-significant plant communities.

Methods

We determined the root dynamics and root lifespan with minirhizotrons with or without irrigation to simulate reduced rainfall scenarios.

Results

We found a major effect of irrigation on the early production (0.24 m m^?2 d^?1 increase), occurrence (97% increase) of cluster roots and only slight effects on lifespan (~10 days less) of all root types. With irrigation, the resultant greater soil moisture levels increased the deployment of cluster roots. Apart from cluster roots, the dynamics of other roots did not decline at lower soil moisture levels, suggesting that this system shows some resilience to decreased rainfall.

Conclusions

Future research should focus on assessing if climate-altered cluster-root activity may be promoting compositional shifts in plant communities with additional restraining effects on root trait diversity.

     

中国土壤容重特征及其对区域碳贮量估算的意义

容重是土壤最重要的物理性质之一,不仅能反映土壤质量和土壤生产力水平,还是区域尺度土壤碳贮量估算的重要参数。由于野外测定土壤容重费时费力、并且操作过程也容易造成较大的误差,因此,土壤容重在国内外大多数清查数据库中均缺失严重。通过收集和整理中国第二次土壤普查数据、中国生态系统研究网络数据和1980—2014年论文内的中国土壤容重数据(共11845条记录),系统地探讨了中国陆地生态系统土壤容重的整体分布特征、垂直分布特征以及不同土壤类型间的差异。分析结果表明:中国陆地生态系统的土壤容重数据整体呈正态分布,平均值为(1.32±0.21)g/cm~3,中值为1.35g/cm~3;土壤容重随土层深度增加而增加,两者间表现为显著的幂函数关系。土壤容重与有机质含量呈显著的正相关关系,与沙粒含量的负相关关系较弱。此外,不同土壤类型间的土壤容重差异较大,高山土平均容重最低(0.93 g/cm~3),而盐碱土平均容重最高(1.41 g/cm~3)。结果全面阐释了中国陆地生态系统土壤容重的基本特征及其变异规律,其结论还将为准确评估区域乃至全国土壤碳贮量提供重要参数。     

Influence of root density on the critical soil water potential

Estimation of root water uptake in crops is important for making many other agricultural predictions. This estimation often involves two assumptions: (1) that a critical soil water potential exists which is constant for a given combination of soil and crop and which does not depend on root length density, and (2) that the local root water uptake at given soil water potential is proportional to root length density. Recent results of both mathematical modeling and computer tomography show that these assumptions may not be valid when the soil water potential is averaged over a volume of soil containing roots. We tested these assumptions for plants with distinctly different root systems. Root water uptake rates and the critical soil water potential values were determined in several adjacent soil layers for horse bean (Vicia faba) and oat (Avena sativa) grown in lysimeters, and for field-grown cotton (Gossypium L.), maize (Zea mays) and alfalfa (Medicago sativa L.) crops. Root water uptake was calculated from the water balance of each layer in lysimeters. Water uptake rate was proportional to root length density at high soil water potentials, for both horse bean and oat plants, but root water uptake did not depend on root density for horse bean at potentials lower than −25 kPa. We observed a linear dependency of a critical soil water potential on the logarithm of root length density for all plants studied. Soil texture modified the critical water potential values, but not the linearity of the relationship. B E Clothier Section editor     

不同土壤水分条件下土壤容重对玉米根系生长的影响

用玉米作为实验材料进行分根实验。种子根平分在装有土娄土的分隔的白铁皮桶中。土壤容重分 4种处理 :低容重 (两边容重都为 1 .2 0 g· cm-3 )、中容重 (两边容重都为1 .33g· cm-3 )、高容重 (两边容重都为 1 .45g· cm-3 )和混合容重 (一边为 1 .2 0 g· cm-3 ,另一边为 1 .45g· cm-3 )。土壤水分控制在高基质势 (- 0 .1 7MPa)和低基质势 (- 0 .86MPa) 2个水平。结果表明 :当植株生长在高紧实土壤或土壤基质势从 - 0 .1 7MPa降到 - 0 .86 MPa时 ,根长和根干重都显著降低 ;紧实土壤使根长降低的同时还使根的直径增大。然而 ,当植株生长在混合容重土壤中时 ,处在低容重土壤中的根系生长得到加强 ,补偿甚至超补偿高容重土壤中根系生长的不足     

Influence of soil density on root development and growth of oats

Summary Combinations of three grades of density of topsoil and of subsoil in artificial profiles have been used to study the influence of soil density on growth of the roots of oats. The soil was humous sand.The development of roots proved better the less compact the soil is. In the very dense soil rootgrowth was markedly reduced. It is likely that mechanical resistance is the only reason for the restriction of the growth hereby.Whereas a moderate growth of roots was possible even in the most densely packed soil, such a dense subsoil could absolutely not been penetrated by roots coming from a loose topsoil. This is presumably not due to a lack of support in the loose soil, but to an insufficient osmotic pressure in the roots.The hampered rootgrowth in compacted soil limited the uptake of water and nutrients and hereby reduced the development of the tops of plants.     

Dynamics of ammonia-oxidizing communities in barley-planted bulk soil and rhizosphere following nitrate and ammonium fertilizer amendment

Oxidation of ammonia by nitrifying microorganisms is a major pathway that fertilizer nitrogen (N) may take upon application to agricultural soils, but the relative roles of bacterial (AOB) vs. archaeal (AOA) ammonia oxidizers are controversial. We explored the effects of various forms of mineral N fertilizer on the AOB and AOA community dynamics in two different soils planted with barley. Ammonia oxidizers were monitored via real-time PCR and terminal restriction fragment length polymorphism analysis of bacterial and archaeal amoA genes following the addition of either [NH?]?SO?, NH?NO? or KNO?. AOB and AOA communities were also studied specifically in the rhizospheres of two different barley varieties upon [NH?]?SO? vs. KNO? addition. AOB changed in community composition and increased in abundance upon ammonium amendment in bulk soil and rhizosphere, with changes in bacterial amoA copy numbers lagging behind relative to changes in soil ammonium. In both soils, only T-RFs corresponding to phylotypes related to Nitrosospira clade 3a underwent significant community changes. Increases in AOB abundance were generally stronger in the bulk soil than in the rhizosphere, implying significant ammonia uptake by plant roots. AOA underwent shifts in the community composition over time and fluctuated in abundance in all treatments irrespective of ammonia availability. AOB were thus considered as the main agents responsible for fertilizer ammonium oxidation, while the functions of AOA in soil N cycling remain unresolved.     

Incorporating sheep into dryland grain production systems: III. Impact on changes in soil bulk density and soil nutrient profiles

Changes in soil bulk density and soil nutrient profiles are a major concern of dryland grain producers considering grazing sheep on cereal stubble fields. Our objective was to compare burned, grazed, tilled, trampled and clipped wheat stubble fields on changes in soil bulk density and soil nutrient profiles. Treatments were evaluated in a series of three experiments using a randomized complete block design and four replications at each site. Contrast statements were used to make pre-planned comparisons among treatments. For Experiment 1, treatments were fall tilled, fall grazed, spring grazed, fall and spring combined (Fall/Spr) grazed, and an untreated control. Five mature ewes were confined with electric fence to a 111 m² plot for 24 h for fall and spring grazed plots resulting in a stocking rate of 452 sheeps d/ha. For Fall/Spr, the stocking rate was 904 sheeps d/ha. For Experiment 2, treatments were fall grazed, fall burned, fall tilled, and an untreated control. In Experiment 3, treatments were fall trampling by sheep, spring trampling by sheep, fall and spring combined (Fall/Spr) trampling by sheep, hand clipping to a stubble height of 4.5 cm, and an untreated control. Trampling treatments were done at the same stocking rates as grazing treatments but sheep were muzzled to prevent intake. In Experiment 1, post-treatment organic matter tended to be greater (P = 0.09) in the mean of the grazed treatments than control plots. In all of the experiments, change in soil bulk density, and soil nutrient profiles did not consistently differ (P > 0.07) among treatments in any manner that would suggest a detrimental impact of grazing sheep on small grain residue. These results indicate a strong potential for grazing sheep on grain stubble without adversely impacting soil bulk density or nutrient profiles.     

Influence of bulk and tapped density on the determination of the thermal conductivity of powders and blends

The aim of this study was to evaluate a non-steady-state needle sensor to determine the thermal conductivity (lambda) of powders and their blends. It was investigated how lambda of different powders was influenced by (1) bulk vs tapped density, (2) moisture content of the powders, and (3) blending time of the powders. Different powders were evaluated: 2 lactose powders with different properties, a microcrystalline cellulose powder, a cornstarch powder, and 3 herbal extracts. The results show that the values of lambda are highly dependent on the bulk and tapped density of the powders. Bulk density measurements were generally not sensitive enough to detect the moisture content within a powder. The tapped density measurements were reliable and highly reproducible and could differentiate between the nature of a powder and the powder moisture content. Measurements of lambda were able to be used to monitor the powder blending process. To be able to use thermal conductivity measurements to characterize powder properties in quality control, the powder density must be defined because changes in density affect lambda. Using thermal conductivity as a measure for process analytical technology seems to be feasible and can add valuable information to the process under investigation.     

黄土高原小流域土壤容重及水分空间变异特征

在黄土高原小流域尺度上,地形和土地利用是影响土壤变异的重要因素.在横山县朱家沟小流域采集了82个样点,选取土壤容重和水分作为研究对象,分析比较不同土地利用及不同景观位置下二者的变异及分布特征;分析了土壤容重和水分与地形因素的关系并利用地形与土地利用信息进行了回归分析.结果表明,不同土地利用类型之间,土壤容重变异较小,其大小次序为：灌木林地＞荒草地＞梯田＞坝地＞林地＞坡耕地;土壤水分变化相对较大,大小次序为：坝地＞荒草地＞灌木林地＞坡耕地＞林地＞梯田.在不同景观位置,土壤容重大小变化表现为：坡顶＞沟平地＞坡下＞坡上＞坡中;土壤水分大小变化为：沟平地＞坡中＞坡下＞坡上＞坡顶.基于数字地形分析技术,提取相关地形指数,与土壤容重和水分进行相关分析并进行多元回归分析,结果表明：土壤容重与复合地形指数CTI正相关;土壤水分与高程呈现负相关关系,和剖面曲率正相关.建立了多元线性回归模型,结果发现模型对土壤容重预测结果比较理想,但对于土壤水分的预测存在较大的平滑效应,残差较大,须进一步探讨.     

The effect of soil warming on bulk soil vs. rhizosphere respiration

There has been considerable debate on whether root/rhizosphere respiration or bulk soil respiration is more sensitive to long-term temperature changes. We investigated the response of belowground respiration to soil warming by 3 °C above ambient in bare soil plots and plots planted with wheat and maize. Initially, belowground respiration responded more to the soil warming in bare soil plots than in planted plots. However, as the growing season progressed, a greater soil-warming response developed in the planted plots as the contribution of root/rhizosphere respiration to belowground respiration declined. A negative correlation was observed between the contribution of root/rhizosphere respiration to total belowground respiration and the magnitude of the soil-warming response indicating that bulk soil respiration is more temperature sensitive than root/rhizosphere respiration. The dependence of root/rhizosphere respiration on substrate provision from photosynthesis is the most probable explanation for the observed lower temperature sensitivity of root/rhizosphere respiration. At harvest in late September, final crop biomass did not differ between the two soil temperature treatments in either the maize or wheat plots. Postharvest, flux measurements during the winter months indicated that the response of belowground respiration to the soil-warming treatment increased in magnitude (response equated to a Q ₁₀ value of 5.7 compared with ∼2.3 during the growing season). However, it appeared that this response was partly caused by a strong indirect effect of soil warming. When measurements were made at a common temperature, belowground respiration remained higher in the warmed subplots suggesting soil warming had maintained a more active microbial community through the winter months. It is proposed that any changes in winter temperatures, resulting from global warming, could alter the sink strength of terrestrial ecosystems considerably.     

The effect of sulphide on nitrate reduction in soil

Summary Soil, amended with sodium sulphide, was incubated anaerobically with added nitrate, and the nitrogenous endoproducts-gaseous-N, nitrate-, nitrite- and ammonium-N—measured.Sulphide depressed gaseous-N production (denitrification), but stimulated the reduction of nitrate to ammonium, and, to a lesser extent, to nitrite.Saskatchewan Institute of Pedology Publication No. R84.     

Influence of soil applications of nitrogen on nitrate reductase activity,leaf and grain protein content in sorghum

Summary Three sorghum genotypes, L.187, SK5912 and RCFA×L.187 (the latter being a hybrid) were field grown under four nitrogen application rates and replicated four times. The experiments were of complete randomized plot design and conducted in 1976, 1977 and 1978.Nitrate Reductase Activity (NRA) was measured at 5, 7, 9, 11, 13, and 15 weeks and at 18, 19, 20 and 21 weeks after planting in 4th vegetative leaf and flag leaf respectively. Flag leaf, 4th leaf and grain protein contents were also measured.Nitrogen application generally increased NRA in both 4th leaf and flag leaf in the 3 genotypes at all the sampling dates.NRA of the hybrid, RCFA×L.187 was consistently higher than those of SK5912 and L.187 (both straight varieties).NRA of 4th leaf was negatively correlated with leaf protein but flag leaf protein tended to increase with applied nitrogen.Flag leaf NRA was positively and significantly correlated with grain protein indicating an important part played by the flag leaf relative to protein accumulation of the developing grain.     

Root penetration through a high bulk density soil layer: differential response of a crop and weed species

Weed control remains one of the greatest problems in agro-ecological systems. An important factor controlling crop and weed competition for below ground resources is the presence of compacted soil layers or ‘hard pans’. In a series of experiments, we investigated the ability of roots of soybean (Glycine max L.) and the weeds sicklepod (Senna obtusifolia L.) and Palmer amaranth (Amaranthus palmeri S. Wats) to penetrate through a compacted soil layer and acquire N from lower in the soil profile. Soil columns were constructed to simulate a compacted soil layer with different bulk densities ~8 cm beneath the soil surface. Results indicated that roots of the two weed species penetrated high bulk density soil layers more effectively than those of four soybean lines. Root penetration was not related with growth rates among the species or soybean genotypes. Overall root and shoot growth of the weeds was sustained when downward root growth was inhibited, while both declined with soybean, even under high fertility conditions. The weeds also acquired relatively high amounts of $^{15} {\text{N}} - {\text{NO}}_{\text{3}}^ - $ from buried patches beneath the high bulk density layers compared to soybean. The results indicate that the weed species would have a competitive advantage when plow pans are present, and an attempt is made to relate this advantage with competitive dynamics observed in the field.     

Exploring the interacting effect of soil texture and bulk density on root system development in tomato (Solanum lycopersicum L.)

Knowledge of the responses of root systems in horizoned heterogeneous soil is vital to optimise uptake of water and nutrients to maximise crop productivity. We explored the interacting effects of soil bulk density and texture on the development of root systems in tomato.Two main techniques were employed, X-ray micro-Computed Tomography (μCT), to provide non-destructive, three-dimensional (3D) images of root systems in situ and destructive root washing followed by WinRHIZO^® scanning. Solanum lycopersicum L. cv. Ailsa Craig plants were grown in soil columns for 10 days to measure the effect of soil compaction on selected root traits. Treatments included bulk density (1.2–1.6 Mg m⁻³), soil texture (loamy sand and clay loam) and the effects of layering.The effect of bulk density on root growth was greatest 3 days after transplanting (DAT) in both soil types. The effect of soil texture was not apparent at this stage, but was significant at 10 DAT for most root and shoot variables. The influence of bulk density differed between soil types as increasing compaction promoted plant growth in clay loam but retarded root growth in loamy sand.We observed that at 3 DAT root growth is primarily influenced by bulk density but by 10 DAT a switch in the processes regulating root growth occurs and the texture of the soil becomes very influential. Future investigations of root growth must consider soil physical properties individually and at specific time points, as their importance changes as the root system becomes established. Here we have demonstrated both positive and negative impacts across a wide range of bulk density treatments in different soil textures on root growth. This illustrates the importance of understanding the complex nature of root–soil interactions, especially for agricultural practices such as seedbed preparation.     

Nitrification and nitrate dissimilation in soil

Summary 1. Studies were made on the decomposition of a substrate containing glucose, ammonia, and nitrate in soil held under differing aeration conditions.2. When water slurries were incubated with substrate, the loss of total-N equalled the loss of nitrate plus nitrite nitrogen.3. Under percolation conditions, with small amounts of substrate and an oxygen partial pressure of 15.2 cm of mercury, there was little change in nitrate or nitrite concentrations. Loss of nitrate only occurred under conditions of reduced aeration but, when it did occur, the sum of nitrate plus atmospheric oxygen utilized by the soil was approximately the same, irrespective of the loss of nitrate. Under an atmosphere of oxygen-free nitrogen, gas output was proportional to loss of nitrate plus nitrite nitrogen. In all cases immobilisation of ammonia was similar.4. Soils which had been percolated under anaerobic conditions with substrate, when put under aerobic conditions and with fresh substrate added, did not lose nitrate. Soils that had been percolated under aerobic conditions, when put under anaerobic conditions and with fresh substrate added, lost nitrate after a lag phase. The period of the phase was decreased by using small amounts of substrate for the aerobic percolation.5. It is concluded that analyses for nitrate and nitrite, or measurements of oxygen uptake, can be used to give approximate measures of nitrate dissimilation.