Fixed Ammonium Content and Maximum Capacity of Ammonium Fixation in Major Types of Tillage Soils in Hunan Province, China

In order to understand the status of fixed ammonium, fixed ammonium content, maximum capacity of ammonium fixation, and their influencing factors in major types of tillage soils of Hunan Province, China, were studied with sampling on fields, and laboratory incubation and determination. The main results are summarized as follows: (1) Content of fixed ammonium in the tested soils varies greatly with soil use pattern and the nature of parent material. For the paddy soils, it ranges from 135.4 ± 57.4 to 412.8 ± 32.4 mg kg⁻¹, with 304.7 ± 96.7 mg kg⁻¹ in average; while it ranges from 59.4 to 435.7 mg kg⁻¹, with 230.1 ± 89.2 mg kg⁻¹ in average for the upland soils. The soils developed from limnic material and slate had higher fixed ammonium content than the soils developed from granite. The percentage of fixed ammonium to total N in the upland soils is always higher than that in the paddy soils. It ranges from 6.1 ± 3.6% to 16.6 ± 4.6%, with 14.0% ± 5.1% in average for the paddy soils and it amounted to 5.8 ± 2.0% to 40.1 ± 17.8%, with 23.5 ± 14.2% in average for upland soils. (2) The maximum capacity of ammonium fixation has the same trend with the fixed ammonium content in the tested soils. For all the tested soils, the percentage of recently fixed ammonium to maximum capacity of ammonium fixation is always bellow 20% and it may be due to the fact that the soils have high fertility and high saturation of ammonium-fixing site. (3) The clay content and clay composition in the tested soils are the two important factors influencing their fixed ammonium content and maximum capacity of ammonium fixation. The results showed that hydrous mica is the main 2:1 type clay mineral in <0.02 mm clay of the paddy soils, and its content in 0.02–0.002 mm clay is much higher than that in <0.002 mm clay of the soils. The statistical analysis showed that both the fixed ammonium content and the maximum capacity of ammonium fixation of the paddy soils were positively correlated with the total 2:1 type clay mineral content and hydrous mica content in <0.02 mm clay and 0.02–0.002 mm clay at the significant level of P_0.01 or P_0.05, respectively, but not correlated with the total 2:1 type clay mineral content and hydrous mica content in <0.002 mm clay significantly. It demonstrated that the ammonium-fixing matrix of the tested soils mainly exists in the 0.02-0.002 mm clay. The above-mentioned results showed that fixed ammonium is a major form of N in the tillage soils in Hunan Province, China. It would play an important role in N nutrition of crops, especially for upland crops, and deserve to be further researched.     

黄河乌兰布和沙漠段沿岸沙丘形态及其运移特征

为更合理、精确地计算黄河乌兰布和沙漠段的入黄沙量,探明其对黄河沿岸植被造成的影响程度,以黄河乌兰布和沙漠段沿岸沙丘为研究对象,通过野外地貌调查、沙丘形态测量和遥感解译对其沙丘的形态特征及其运移特征进行了系统研究。结果表明:乌兰布和沙漠沿黄段沙丘以走向西南—东北的新月型沙丘和新月型沙丘链为主,沙丘剖面形态不对称,具有明显落沙坡;在发育过程中同时受到了西南风和西北风的显著影响,5年内以沙丘整体向河道推进为主,共移动19.45m,具有单向快速运移的特点,且沙丘不断向黄河侵袭,应采取措施予以遏制。     

Spatial pattern and heterogeneity of soil properties in sand dunes under grazing and restoration in Horqin Sandy Land, Northern China

Applying a combination of classical and geostatistical methods, we identified soil properties and their spatial variation in a 5-year grazed sand dune (GSD5) and a 20-year recovered sand dune (RSD20) in Horqin Sandy Land, northern China. The paper assesses the effect of grazing, topography and vegetation restoration on spatial heterogeneity of soil properties. The results showed that soil organic carbon, total nitrogen, very fine sand (0.1–0.05 mm) content and their coefficients of variation were lower in GSD5 than in RSD20, while soil water contents (0–20 cm and 20–40 cm depths) were higher in GSD5 than in RSD20. Geostatistical analysis revealed that the spatial structured variance accounted for the largest proportion of total sample variance in soil properties at the measured scale under grazing and restoration. The spatial autocorrelation ranges were 66.30 m for soil organic carbon and 50.80 m for total nitrogen in GSD5 less than those in RSD20 (70.00 m and 76.10 m, respectively), while the spatial autocorrelation ranges of soil particle size fractions and soil water contents in RSD20 were less than those in GSD5. Kriging-interpolated maps also showed that the heterogeneity of soil organic carbon and total nitrogen and their degree of patch fragmentation were higher in GSD5 than in RSD20. These results suggested that continuous grazing resulted in an increase in spatial variability of soil nutrient and a decrease in spatial variability of soil particle size fractions and soil water content. Soil organic carbon and total nitrogen of sand dunes are associated closely with soil particle size fractions, relative height of sampling site and vegetation cover. Spatial patterns of soil properties are most strongly related to grazing, topography and plant-induced heterogeneity in sand dune ecosystems prone to wind erosion.     

积的压缩映象的某些不动点定理

在完备度量空间上研究了可换积的压缩映象,从而建立了若干不动点定理,证明了不动点存在性、唯一性。它们是参考文献「１」－「４」的主要结果的改进、统一和发展。     

森林经理工作的形势与对策建议

分析了国有林区森林经理工作所面临的形势与要求 ,就区划林种经营固定小班 ,森林资源调查的深度、质量与方法 ,编制局场两级森林经营方案 ,建立林种小班森林经营档案 ,建立森林经理工作制度 5个问题 ,提出了相应的对策和改革建议     

给定行程速度变化系数的四杆机构设计

在一些教科书中,对于给定行程速度变化系数的四杆机构设计,结论上存在一些错误和缺陷。利用几何方法,对曲柄中心所在位置的各种可能性进行了分析,给出了较为完整的结论。     

长期定位施不同氮源有机肥替代部分含氮化肥对陇东旱塬冬小麦产量和水分利用效率的影响

在陇东黄土旱塬覆盖黑垆土大田,利用陇鉴301进行了连续10年的定位试验,观测长期施用不同氮源有机肥(发酵有机肥、农家肥)或小麦秸秆还田各处理对冬小麦产量相关性状和水分利用效率的影响。结果显示,小麦产量和水分利用效率年际间变化较大,与降雨量有直接关系;不同有机氮源替代部分含氮化肥处理对提高冬小麦产量和水分利用效率具有明显作用。在干旱、平水和丰水年型,较不施肥对照分别增产53.1%~103.7%、40.3%~79.3%和73.1%~94.8%,较单施化肥对照分别增产6.6%~41.8%、7.0%~36.8%和-2.9%~9.3%。以发酵有机肥做替代物处理的产量和水分利用效率最高,增产幅度最大,10年平均产量较不施肥和单施化肥对照分别增加88.9%和25.4%,水分利用效率和边际水分利用率也最高,分别为10.8 kg mm~(-1) hm~(-2)和1.03 kg m~(-3);并且产量构成因素和植株生理指标也优于其他处理。因此,发酵有机肥是陇东半湿润偏旱雨养农业区(年降水量约550 mm)冬小麦生产上替代部分含氮化肥的首选有机氮源。     

石灰性土壤中磷肥后效的研究

通过五年田间定位试验的结果表明,磷肥具有明显而持久的后效。后效的大小和持续时间主要取决于磷肥的施用量;后效持续的时间与磷肥施用量之间是指数函数关系;当施磷处理耕层土壤速效磷水平降至与对照处理基本相同时,磷肥后效即告结束。     

黄家二岔小流域土壤水分空间分布特征

该文采用定位观测和谐波分析的方法对黄家二岔小流域土壤水分空间分布特征进行了研究．结果表明： 无论何种降雨年型, 流域内中游地段土壤含水量最高, 下游地段土壤含水量高于上游, 坡下部的高于坡上部, 阴坡高于阳坡．