Landscape and Land‐Use Effects on the Spatial Variation of Soil Chemical Properties     

《Communications in Soil Science and Plant Analysis》2012,43(15-16):2389-2412

The current study addressed the spatial variation of soil organic matter (SOM), total nitrogen (TN), extractable phosphorus (EP), and extractable potassium (EK) in agricultural soils of a representative region, northeast China. Soil cation exchange capacity (CEC) and the effects of landscape attributes and land use were also investigated. The techniques used included conventional statistics, geostatistics, and geographic information systems (GIS). Our study demonstrated that EP had the greatest coefficient of variation (CV), and CEC had the least CV. The experimental semivariograms of the five soil chemical properties included in this study were all fitted with exponential models. The five soil variables all showed moderate spatial dependence. The SOM, EK, and CEC decreased with increasing altitude. Significant negative relationships were found between the slope gradient and EP, EK, and CEC. Relatively steeper slopes might result in greater soil erosion, which leads to a decline in soil nutrients. Soil types had significant impacts on all soil chemical properties, which reflect the effect of the parent soil material. In general, the mean values of soil variables for vegetable land were statistically greater than those for upland and paddy fields. After being divided into two parts along the Yinma River, soil samples of the western part have statistically greater SOM, EP, EK, and CEC values than those collected from the eastern part.  相似文献   

重金属锌对猪粪堆肥过程中氧化还原类酶活性的影响     

张卫娟  谷洁  高华  张洪宾  刘强  李海龙 《农业环境保护》2011,(2):383-388

以猪粪和秸秆为主要试验材料,添加不同浓度重金属Zn,采取发酵罐处理方法,在好氧高温条件下研究了重金属Zn对猪粪堆肥过程中多酚氧化酶、脱氢酶活性的变化,以及堆腐过程堆体温度、堆料pH值、胡敏酸E4/E6值的变化。结果表明：（1）低量重金属Zn处理（L）较不添加重金属Zn（CK）和添加高量重金属Zn（H）堆料升温快、温度高、高温持续时间长。（2）重金属Zn的加入对堆料的pH值影响不大,不是影响堆肥进程的直接原因。（3）H处理在整个堆肥过程中E4/E6值均高于L和CK,表明高浓度Zn处理抑制腐殖质的缩合和芳构化。（4）L处理的多酚氧化酶活性大多数时间高于H处理的活性,说明低量重金属Zn更好地促进了木质素的降解及其产物的转化。（5）从整个堆肥过程来看,3个不同处理的脱氢酶活性表现出一定的不稳定性,可能是重金属对脱氢酶活性有抑制作用的同时发生＂抗性酶活性＂现象。  相似文献   

黄山风景区步道土壤理化性质变化特征分析   总被引：4，自引：0，他引：4  

韦大山  方凤满  杨仲元 《水土保持研究》2012,19(2):175-179

步道作为旅游景区重要的基础设施之一,是旅游活动冲击的主要对象,尤其以步道两侧土壤环境受影响最为显著。在黄山风景区内选择7条主要步道,设置14条调查样带,每条样带按照距游道远近依次选取5个连续样方,每个样方的面积设置为1 m×1m。在野外调查和实验室分析的基础上,采用多重比较等方法并建立土壤影响指数模型来探讨旅游活动对黄山风景区土壤环境的影响程度和规律。结果显示:旅游活动对土壤的硬度、pH值、有机质、全磷、全钾等因子的变化有显著的影响,其受影响范围主要集中在距步道4m内;由于游客访问比例不同,不同步道受影响的程度有明显差异,其中以玉屏景区和北海景区受影响较为严重,天海景区和西海景区次之,上山道和下山道受影响最小。  相似文献   

煤矿矿区不同采煤塌陷年限土壤物理性质对比研究   总被引：8，自引：0，他引：8  

谢元贵  车家骧  孙文博  彭熙 《水土保持研究》2012,19(4):26-29

为揭示采煤塌陷对矿区土壤物理性质的影响机理,为矿区生态修复和重建提供理论依据,在选取典型样地的基础上,采用土壤测定方法,研究了不同塌陷年限不同土层土壤物理性质的变化。结果表明:随采煤塌陷年限的延长,矿区表层土壤密度逐渐增大,底层土壤密度先增大后减小;毛管孔隙度逐渐下降,非毛管孔隙度先下降后上升;表层土壤总孔隙度逐渐下降,底层土壤总孔隙度先下降后上升;土壤体积含水量和土壤贮水量先上升后下降,土壤质量含水量逐渐下降;表层土壤毛管持水量逐渐降低,底层土壤毛管持水量先下降后上升;表层土壤田间持水量逐渐降低,底层土壤田间持水量先下降后上升;土壤排水能力先下降后上升。  相似文献   

大庆龙凤湿地土壤理化性质与硒元素分布关系研究   总被引：5，自引：0，他引：5  

陈雪龙  王晓龙  齐艳萍 《水土保持研究》2012,19(4):159-162

为了解大庆龙凤湿地土壤理化性质对硒的含量、形态与分布的影响,对大庆龙凤湿地保护区4个样区20个样点4个不同层次土样中硒的含量、形态、分布以及部分理化性质进行了研究。结果表明:大庆龙凤湿地土壤全硒含量为121～150μg/kg,由于硒淋溶流失的影响,随土壤深度的增加,全硒含量无明显变化;有效硒总量为22～28μg/kg,包括水溶态硒、交换态硒与富啡酸态硒三种形态。影响土壤硒的主要因素包括土壤有机质、土壤黏粒含量及pH值,其中土壤有机质、黏粒含量与硒含量之间存在正相关关系,土壤pH值与硒含量存在极显著的负相关关系。  相似文献   

Response of soil properties and yam yield to Chromolaena odorata (Asteraceae) and Tithonia diversifolia (Asteraceae) mulches     

Taiwo M. Agbede  Aruna O. Adekiya  Joseph S. Ogeh 《Archives of Agronomy and Soil Science》2013,59(2):209-224

Plant materials differ in their chemical composition, rate of decomposition and suitability as mulch materials. Experiments were conducted during 2006–2007 and 2007–2008 cropping seasons for early yam cultivation at Owo in the forest–savanna transition zone of southwest Nigeria to study the effect of Chromolaena odorata and Tithonia diversifolia mulches applied at 0.0, 5.0, 7.5, 10.0 and 12.5 t ha^?1 on soil chemical properties, leaf nutrient composition, growth and tuber yield of white yam (Dioscorea rotundata Poir). Both C. odorata and T. diversifolia mulches reduced soil bulk density and temperature; increased concentrations of soil organic matter (SOM), total N, available P, exchangeable K, Ca and Mg, leaf N, P, K, Ca and Mg; enhanced growth and yield of yam compared with control. The values of SOM, total N and available P and leaf N and P concentrations increased with increasing mulch rate. C. odorata mulch and T. diversifolia mulch applied at 10.0 and 7.5 t ha^?1, respectively, was found to be suitable for yam production. T. diversifolia mulch compared with C. odorata mulch produced higher values of soil chemical properties, leaf nutrient concentrations, growth and yield of yam. T. diversifolia mulch produced 19% and 18% higher tuber yield compared with C. odorata mulch during 2006–2007 and 2007–2008 cropping seasons, respectively.  相似文献   

秸秆生物反应堆与菌肥对温室番茄土壤微环境的影响   总被引：7，自引：3，他引：7  

孙婧  田永强  高丽红  彭杏敏  佟二建 《农业工程学报》2014,30(6):153-164

为研究秸秆生物反应堆、微生物菌肥及两者配套措施对土壤理化性质和微生物功能多样性,以及作物生长的长期影响,试验以传统种植方式为对照(CK,常规栽培),研究了菌肥(T1,微生物菌肥4 kg/667 m2)、内置式秸秆生物反应堆(T2,秸秆(4 t/667 m2)+发酵沟菌剂(8 kg/667 m2)+腐熟猪粪(600 kg/667 m2))及2种措施配套处理(T3,秸秆(4 t/667 m2)+发酵沟菌剂(8 kg/667 m2)+微生物菌肥(4 kg/667 m2)+腐熟猪粪(600 kg/667 m2))对土壤理化性质和微生物功能多样性的影响。结果表明:1)与CK相比,秸秆生物反应堆能够在一定时期内提高土壤含水率;而菌肥能够在一定时期内降低土壤含水率,秸秆生物反应堆能够显著降低土壤酸性和电导率(EC,electrical conductivity)值,缓冲土壤酸化和次生盐渍化;而单施菌肥对土壤酸碱性和EC值没有显著影响。2)秸秆生物反应堆(T2)增加了土壤中有机质的含量和土壤微生物量,降低土壤中速效磷、钾的含量;微生物菌肥(T1)降低了土壤中有机质含量和微生物量,而显著提升了土壤的速效磷、速效钾含量,两种措施配套处理效果则更明显。3)菌肥能够改善土壤微生物对多聚物、碳水化合物和氨基酸的利用效率,而秸秆生物反应堆能够促进土壤微生物对于一部分氨基酸、羧酸类、酚酸类和胺类物质的利用。而2种措施同时使用时,其促进和改善微生物碳代谢能力的作用则更加显著。4)各处理均能够在一定程度上增加各年度番茄产量。综合考虑,认为内置式秸秆生物反应堆和菌肥配套处理(T3)能够更好的改善和修复日光温室连作土壤,增加作物产量,是一种较为有效的农艺措施。  相似文献   

不同类糖接枝改性对花生蛋白膜物理性质的影响   总被引：1，自引：0，他引：1  

林伟静  刘红芝  刘丽  石爱民  胡晖  王强 《农业工程学报》2014,30(11):261-267

为了改善花生蛋白膜的性能,利用不同小分子糖对花生蛋白进行接枝改性并将改性蛋白制备成膜,分析了糖接枝对花生蛋白膜的强度、延伸性、透光性、溶解性等物理性质的影响。结果表明:糖类物质能提高花生蛋白膜的拉伸强度,其中木糖改性后蛋白膜强度最高,达未经改性花生蛋白对照膜的1.77倍;葡萄糖对蛋白膜的延伸性影响最大,断裂延伸率最高,达对照膜的1.92倍;木糖能改善花生蛋白膜的耐水性,使膜的溶解性显著下降。综合来看,木糖接枝改善花生蛋白膜性能的效果较好,当蛋白/木糖质量比为10时,蛋白膜拉伸强度为1.48 MPa,断裂延伸率为218.92%,溶解性60.80%,蛋白膜浸泡24 h后仍保持完整膜状态。该研究为花生蛋白膜的性能改善以及进一步开发利用提供理论依据。  相似文献   

Role of active aluminum in the formation of water-stable macroaggregates     

Saiyed Md. Ibrahim  Yoshiaki Inoue  Haruo Shindo 《Soil Science and Plant Nutrition》2013,59(4):685-689

Soil structure is determined by the arrangement of particles in soil and the particles of sand, silt, and clay bind together into aggregates of various sizes by organic and inorganic materials. Structural stability which is the ability of the aggregates and pores to remain intact when subjected to stress, markedly affects crop production and soil erosion (Tisdall 1996). Since water, either directly as rainfall or as surface runoff is the main agent of aggregate breakdown, in the analyzes of stable soil aggregation, the term water-stable aggregation is generally used (Lynch and Bragg 1985). Water-stable aggregates have been divided into micro aggregates < 0.25 mm dia.) and macro aggregates (> 0.25 mm dia.) (Edwards and Bremner 1967; Tisdall and Oades 1982). Microaggregates show a relatively high stability against physical disruption (Edwards and Bremner 1967). On the other hand, macro aggregates are sensitive to soil management (Tisdall and Oades 1982).

There are many reports on the relationships between the aggregate stability and the soil physicochemical properties. For example, significant correlations were found between the aggregate stability and the amounts of organic C (Tisdall and Oades 1982), total N, and carbohydrates or the CEC (Chaney and Swift 1984). However, most of these studies were conducted in non-volcanic ash soils. Volcanic ash soils are widely distributed in Japan and are very important soils for crop production. The objective of this study was, therefore, to obtain more information on the relationship between the degree of macro aggregation and the soil physicochemical properties in non-volcanic and volcanic ash soils.  相似文献   

Soil amendments and seed priming influence nutrients uptake,soil properties,yield and yield components of wheat (Triticum aestivum L.) in alkali soils     

Zahir Shah  Izhar ul Haq  Abdur Rehman  M. Afzal 《Soil Science and Plant Nutrition》2013,59(2):262-270

The effects of soil amendments [i.e., control, gypsum, farmyard manure (FYM), and gypsum?+?FYM] and seed priming (i.e., unprimed, seed soaked in water for 10?hr prior to sowing, and seed soaked in 0.4% gypsum solution for 10?hr prior to sowing) were assessed on growth and yield of wheat (Triticum aestivum L.) crop in alkali soil in northwestern Pakistan. A split plot design was used, keeping priming methods in main plots and soil amendments in sub-plots. The results showed that the effects of soil amendments and seed priming on grain yield, straw yield, harvest index and number of spikes were significant but their interactive effect was non-significant. The highest crop yields and yield index were obtained with gypsum?+?FYM amendments, and seed priming with gypsum solution. The effect on seed emergence, plant height and number of grains per spike was, however, not significant. Grain yield increased by 104% in gypsum?+?FYM treatment over control and by 16.8% with seed primed in water, followed by 8.5% with priming in gypsum solution, as compared to non-priming. The weight of 1000 grains was significantly increased by 35% in gypsum?+?FYM treatment and by 15.8% in gypsum priming. The phosphorus (P) and potassium (K) content increased with soil amendments. Soil pH and gypsum requirement reduced significantly with soil amendments. The blend of gypsum and FYM has improved the properties of salt-affected soil and enhanced fertility for optimum production of wheat in addition to the beneficial effect of seed priming in gypsum solution on crop yield. Using these amendments could be ameliorative in removing the adverse effect of the salt-affected soils, rendering the soil a good medium for plant growth.  相似文献