条施调酸材料对石灰性土壤调酸及马铃薯锌硼吸收的影响

【目的】研究条施调酸材料的调酸效应及其对马铃薯锌、硼吸收的影响,为调酸材料在马铃薯上的应用提供依据。【方法】以马铃薯为材料,采用田间试验,设置根区施用磷酸一铵（MAP）、硫磺(S)、混合调酸剂(磷酸一铵和硫磺按质量比1∶1混合,MS）,以不施用调酸材料为对照,分析调酸材料施入石灰性土壤后土壤pH值、锌硼有效性以及马铃薯叶片、块茎锌硼含量的变化,研究3种调酸材料根区条施后的调酸效应及对土壤锌硼有效性和马铃薯锌硼吸收的影响。【结果】施入调酸材料能显著降低石灰性土壤pH值,在马铃薯整个生育期调酸效应总体表现为MS＞MAP＞S。施用调酸材料能提高淀粉积累期马铃薯根区土壤有效锌和有效硼含量,MAP、S、MS处理土壤有效锌含量较对照分别提高了58.82%,9.80%和37.25%,土壤有效硼含量较对照分别提高了53.01%,57.83%和61.45%。施用调酸材料后,苗期马铃薯叶片锌、硼积累量分别增加了48.44%~60.83%和40.73%~58.68%,块茎膨大期分别增加了31.43%~39.88%和22.40%~33.06%;在淀粉积累期,MS和S处理马铃薯叶片锌积累量较对照分别降低了51.85%和30.25%,而MAP处理则较对照增加了4.79%,MAP、S、MS处理马铃薯叶片硼积累量较对照分别减少了20.67%,41.78%和38.21%。收获期施用调酸材料后,MAP、S、MS处理马铃薯块茎锌含量较对照分别降低了9.47%,4.94%和14.81%,S、MS处理马铃薯锌积累量较对照分别降低了5.88%和21.08%,而MAP处理提高了30.39%;MAP、S、MS处理马铃薯块茎硼含量较对照分别提高了14.97%,15.51%和63.10%,硼积累量分别提高了67.74%,16.13%和51.61%。【结论】调酸材料降低了石灰性土壤pH值和马铃薯块茎锌含量,但提高了马铃薯块茎硼含量;从调酸效应和马铃薯块茎吸收来看,磷酸一铵与硫磺配施最有利于马铃薯对土壤中微量元素锌硼的利用。     

植酸酶对生长猪植物性饲料中磷利用率的影响

试验采用 4× 4拉丁方设计 ,设两组 ,以 8头始重为 35～ 4 0kg的杜长二元杂种阉猪为试材 ,运用平衡试验法 ,研究植酸酶对小麦、稻谷和高粱三种植物性饲料中磷利用率的影响。试验结果表明 :①利用体重为 35～ 70kg的杜长二元杂种阉猪 ,测得添加植酸酶使小麦中总磷表观消化率提高 2 7 6 4 % ,高梁中总磷表观消化率提高 4 7 87% ,稻谷中总磷表观消化率提高 4 1 84 % ,多重比较差异均极显著 (P <0 0 1) ;磷的沉积率分别是小麦提高 2 7 98% ,高粱提高 4 7 35 % ,稻谷提高 4 0 6 3% ,多重比较差异均极显著 (P <0 0 1) ;②以每天饲喂1kg饲粮计算 ,添加植酸酶使饲喂小麦饲粮的试猪粪磷含量减少 4 9 0 5 % ,饲喂高粱饲粮的试猪粪磷减少5 2 88% ,饲喂稻谷饲粮的试猪粪磷减少 5 8 82 % ;③试验中 5 0 0FTU/kg日粮的植酸酶浓度可使小麦中 5 5 5 5 %、高梁中 5 6 0 0 %、以及稻谷中 6 1 85 %的不可消化磷转变成可消化磷。     

华北落叶松和白杄幼苗对光照和竞争响应的差异比较

选用3年生华北落叶松和白杆幼苗为试验材料,盆栽试验以自然光照为基础设置4个遮光率水平作为不同光照条件,设置5个密度水平,每个树种15个栽植组合方式(包括单独栽植和混合栽植),进行一个生长季节的试验和取样观测分析,以确定这2个树种在苗期对光照和栽植密度的生长和生理响应以及存活率等功能特性的差异.结果表明:华北落叶松幼苗的相对地径生长量在微光条件下显著提高,且其存活率在半光照和弱光照条件下也显著提高.白杆幼苗的高生长量及叶片叶绿素含量表现出随光照减弱而升高的趋势,但其存活率不受光照条件的影响;在不同的栽植密度下,华北落叶松幼苗的生长和生理指标均未表现出显著差异,但适中的栽植密度可显著提高其存活率;白杆幼苗高生长量及叶片叶绿素含量在与落叶松混栽时比单树种栽植时高,但其存活率没有任何变化.上述结果表明:适度遮荫和密植可以在一定程度上改善华北落叶松苗期生长并显著提高其存活率,从而有利于华北落叶松成功度过幼苗幼树期;同时,适度遮荫和混栽也有利于白杆幼苗幼树的生长.     

Relationships between soil and foliar nutrients in young densely planted mini-plots of Pinus radiata and Cupressus lusitanica

The long-term nature of forest crop rotations makes it difficult to determine impacts of forestry on soil nutrients that might be depleted by forest growth. We used small scale, highly stocked plots to compress the length of the rotation and rapidly induce nutrient depletion. In the study, two species (Pinus radiata D. Don and Cupressus lusitanica Miller) are compared under two disturbance regimes (soil undisturbed and compacted), and two fertiliser treatments (nil and plus fertiliser), applied in factorial combination at 33 sites, covering the range of climatic and edaphic variation found in plantation forests across New Zealand. To assess our ability to rapidly highlight important soil properties, foliar nutrient concentrations were determined 20 months after planting. It was hypothesised that the densely planted plots, even at a young age, would create sufficient pressure on nutrient resources to allow development of relationships between properties used as indicies of soil nutrient availability and foliar nutrient concentrations. For both species significant relationships between foliar nutrients and 0–10 cm layer soil properties from unfertilised plots were evident for N (total and mineralisable N) and P (total, acid extractable, organic, Bray-2 and Olsen P). With the exception of Ca in C. lusitanica, foliar K, Ca and Mg were correlated with their respective soil exchangeable cation measures. The results thus confirm the utility of the experimental approach and the relevance of the measured soil properties for forest productivity.

In unfertilised plots foliar N and P concentrations in P. radiata exceeded those in C. lusitanica, the differences being eliminated by fertiliser application. Foliar N/P ratios in P. radiata also exceeded those in C. lusitanica. In contrast to N and P, foliar K, Ca and Mg concentrations were all higher in C. lusitanica, the difference being particularly marked for Ca and Mg. P. radiata contained substantially higher concentrations of the metals Zn, Mn and Al than C. lusitanica, whereas the latter contained higher B concentrations. Possible reasons for differences between species in foliar nutrient concentrations are discussed.     

Micro-scale heterogeneity in urban forest soils affects fine root foraging by ornamental seedlings of Buddhist pine and Northeast yew

Urban soils are frequently characterized by a strong heterogeneity caused by intense anthropogenic activity and land use changes. Soil heterogeneity is commonly known to affect tree root development, but little has been detected concerning root foraging by ornamental trees in heterogeneous urban soils at micro-scale. In this study, Buddhist pine [Podocarpus macrophyllus (Thunb.) D. Don] and Northeast yew (Taxus cuspidata S. et Z.) were selected as ornamental tree species for a two-year study. In the first-year, seedlings were cultured under contrasting photoperiods to generate different morphologies. In the second year, seedlings were transplanted to pots filled with soils collected from an urban forest. Controlled-release fertilizers (N-P₂O₅-K₂O, 14-13-13) were evenly broadcasted to a half patch of the pot (heterogeneity) or to both halves (homogeneity) on the surface 5 cm beneath the pot-top at the rate of 0.135 g N seedling⁻¹. In the fertilized heterogeneous patch, larger Buddhist pine seedlings had greater dry weight, length, surface area, volume, number of tips, and morphological foraging-precision in fine roots. Compared to Northeast yew seedlings under natural photoperiod in the first year, those under the extended photoperiod had larger size, greater fine root biomass, and length but lower foraging-precision in the second year. N and P concentrations in second-year fine roots mainly increased with the availability of patches generated by fertilization for both species. In conclusion, the ability to forage for nutrients by ornamental tree seedlings in heterogeneous urban forest soils was species-specific. Buddhist pine seedlings had higher foraging precision in heterogeneous urban soils than Northeast yew seedlings due to their response to the extended photoperiod during culture.     

Effect of soil pore size distribution on plant-available water and least limiting water range as soil physical quality indicators

Soil pore size distribution(SPSD) is one of the most important soil physical properties. This research investigated the relationships of location and shape parameters of the SPSD curves with plant-available water(PAW) and least limiting water range(LLWR) of the light-textured soils at the Torogh Agricultural Research Station in north-eastern Iran. Soil moisture release curve(SMRC), PAW and LLWR in matric heads of 100 and 330 h Pa for the field capacity and location and shape parameters of the SPSD curves of 30 soils with different texture and organic carbon contents were determined, and the variable relationships were statistically analyzed. The results showed that the median equivalent pore diameter(de), mean de, standard deviation(SD*), and skewness of the SPSD curves were significantly correlated with PAW(PAW330) and LLWR(LLWR330) measured in a matric head of 330 h Pa. Decrease in deand increase in the diversity of soil pore size(SD*) increased PAW330 and LLWR330. The SD* values of all the soil samples were lower than the optimal ranges suggested in literature. Neither PAW nor LLWR values were significantly different in the soils with the optimal modal deand those with non-optimal modal de. Optimal values of median and mean equivalent pore diameters and kurtosis of SPSD curves led to a significant improvement of PAW330 and LLWR330 as soil physical quality indicators. It was recommended to revise the optimal ranges for SD* and modal defor future studies.     

苏南经济快速发展区土壤Ni的形态分布影响因素——以昆山市为例

以江苏省昆山市为典型区,通过现场采样及室内分析测定,定量研究了几种因素对农田土壤Ni形态分布的影响。结果表明：（1）土壤有效态Ni含量为1.31 mg.kg-1,土壤全Ni含量为40.95 mg.kg-1,土壤Ni的活化率为3.38%。（2）土壤重金属Ni各形态含量相对大小为残渣态（36.20 mg.kg-1）〉有机质结合态（2.80 mg.kg-1）〉铁锰氧化物结合态（1.31 mg.kg-1）〉可交换态（0.54 mg.kg-1）、碳酸盐结合态（0.10 mg.kg-1）,残渣态含量明显高于其他形态,达88.16%。（3）pH值是影响可交换态Ni含量的最主要因素,达极显著负相关水平;全Ni含量是影响碳酸盐结合态Ni含量、铁锰氧化物结合态Ni含量和残渣态Ni含量的最主要因素,达极显著正相关水平;有机质含量是影响有机质结合态Ni含量的最主要因素,呈显著正相关水平。（4）〈0.01 mm粘粒含量是影响可交换态Ni含量的重要因素,有机质含量是碳酸盐结合态Ni含量的重要影响因素,pH值和有机质含量都是影响铁锰氧化物结合态Ni含量的重要因素,〈0.01 mm粘粒含量、pH值都是影响有机质结合态Ni含量的重要因素,pH值是影响残渣态Ni含量的重要因素。     

饲料中添加包膜氨基酸对异育银鲫生长和体成分的影响

分别进行了两个试验考察包膜氨基酸的作用效果。试验一以硬化油脂、明胶包膜赖氨酸、蛋氨酸，测定了其水中溶失率。结果表明，晶体赖氨酸、硬化油脂、明胶包膜赖氨酸的水中溶失率分别为57．0％、14．3％、21．3％；晶体蛋氨酸、硬化油脂、明胶包膜蛋氨酸的水中溶失率分别为87．7％、19．0％、28．0％，晶体氨基酸经硬化油脂、明胶包膜后，其水中溶失率极显著降低（P〈0．01）；试验二在鱼粉含量为9％的基础饲料（对照组）中分别添加晶体、硬化油脂包膜、明胶包膜的0．23％赖氨酸和0．09％蛋氨酸，饲养平均体重为2．48g的异育银鲫鱼种6周。结果表明，对照组、晶体氨基酸组、硬化油脂包膜氨基酸组、明胶包膜氨基酸组的鱼体增重率分别为169．8％、173．3％、201．4％、200．2％，添加晶体氨酸对异育银鲫的生长无改善（P〉0．10），但添加硬化油脂包膜或明胶包膜氨基酸试验组鱼体增重率为18．6％、17．9％（P〈0．05），饲料系数下降0．28、0．37（P〈0．05），显著促进了异育银鲫的生长。对肌肉营养成分的分析表明，不同处理鱼体肌肉在水分、粗蛋白、粗脂肪、灰分组成方面无显著差异（P〉0．05）。上述研究表明，晶体氨基酸经硬化油脂、明胶包膜处理后，其水中溶失率显著降低，利用性显著提高，在低鱼粉饲料中添加后对异育银鲫具有显著的促生长作用。     

土壤中微量元素的环境化学特性

论述了微量元素在土壤中的迁移、存在状态,探讨了影响微量元素化学行为及生物有效性的主要土壤环境因素,分析了这些元素在土壤中形态转化的机制及平衡状况,为评价土壤中微量元素的变化,提高其生物有效性提供依据。     

营养盐可得性对坛紫菜氮磷吸收、生长及藻红蛋白含量的影响

实验室条件下,研究了N、P浓度、不同化合态N及N∶P比值对坛紫菜(Porphyra haitanensis)N、P吸收速率,以及P浓度对坛紫菜生长速率和藻红蛋白含量的影响。结果表明,随着营养盐浓度的升高,坛紫菜对N、P的吸收速率也随之增高,当无机氮浓度达到100μmol/L时,坛紫菜对N、P的吸收速率趋向接近最大值;当NO3--N∶NH4+-N比值为1∶5时,坛紫菜对N的吸收达到最大值;坛紫菜对P的吸收速率随NO3--N∶NH4+-N比值的减小而略有增大;坛紫菜对N的吸收速率随着N∶P比值的增大而增大,而对P的吸收速率随着N∶P比值的增大而减小;在磷浓度低于12μmol/L的情况下,坛紫菜的生长速率和藻红蛋白含量随着P浓度的升高而增加,高于12μmol/L时,则不再增加。