共查询到19条相似文献，搜索用时 328 毫秒
1.
通过对济阳县生态地球化学调查研究,该区受成土母质来源、土壤类型、地形地貌及其理化性质等因素影响,土壤元素全量、有效量及有效度表现为：低平洼地土壤中K,P,N,Se,Mn,Fe,Zn,Cu和Mo全量较高,P,N,Se和Cu有效量较高,显示为低平洼地为黏质成分的沉积成因特点;而决口扇形地区土壤Cu,Mo,N,Zn,B有效量和全量均偏低。富含有机质,且pH相对较低的潮土中Se,Cu,Mo和B等元素有效度较高,贫有机质、pH相对较高的草甸风沙土中N,Fe,Cu,Mo,B和S等元素有效量较低,但K有效量和有效度均较高。统计分析表明,土壤中K,P,N,S和Cu等元素全量与有效量间具显著正相关性,表明全量是有效量的重要影响控制因素;有机质含量与K,P,Zn,Cu和B有效度间为显著正相关,说明有机质较高有利于土壤元素活化;Fe,P,S,Zn,B和Cu有效度与pH值为显著负相关,表明土壤酸性增强会增加这类元素的生物有效性。 相似文献
2.
通过对高密市耕地表层土壤进行调查,获得了N,P,K,Cu,Zn,Mo,B等7种营养元素全量和有效量,以及pH值和有机质数据,采用数据统计、相关性分析、对比分析等方法,研究有效态地球化学特征及其受控因素。结果表明,元素全量对有效态具有直观制约影响,元素全量与其有效量均呈正相关,与P,K,Cu,Zn有效度呈正相关,表现为协同作用的有N全量对P有效量,P全量对K,Cu,Zn有效量,Cu全量对P,Zn有效量,Zn全量对P,Cu有效量,P全量对K有效量;酸性土壤能够提高N,P,Cu,Zn,Mo元素的生物有效性,碱性土壤能够提高B元素的生物有效性;有机质能够影响土壤营养元素活化,对有效量有一定的促进作用,有机质增加可以不同程度提高K,Zn,B元素的有效度,但会降低N元素的有效度;不同土壤类型的土壤理化性质有所不同,如土壤pH值和有机质的差异,是影响土壤营养元素有效态的重要因素。 相似文献
3.
在山东省昌乐县的乔官镇、五图镇等地区,分布着46处古火山口,是山东省最为典型的新近纪古火山集中分布地区。为获得该地区表层土壤中地球化学元素垂向分布特征,共设计了3条土壤垂向剖面,对土壤中N、P、K、有机质、Se、Mo、Co、Cu、Zn、Cr、Ni等元素的垂向分布特征进行了研究,并对其变异因素进行了分析。同时,为进一步揭示火山区农产品对各元素的富集能力,选取甜瓜、西瓜、西红柿3种特色农产品为研究对象,查明了不同农产品对土壤元素的富集能力。研究结果表明：火山区所取3种农产品,对Se和Zn元素富集系数相对较高,而对重金属元素相对富集系数较低。 相似文献
4.
5.
通过野外采样和室内测定,以日照茶树种植区3个典型茶园为研究对象,每个茶园分别取鸠坑、黄山群体、福鼎大白各3个品种,最终取得9种茶样生长地的土样,研究分析土样的pH,有机质,全N,P,K,有效N,P,K等指标的土壤养分含量状况,并以此为评价指标,运用模糊综合评判法,对3个茶园的土壤肥力质量进行了综合评价。结果表明,茶园肥力综合水平为北垛春>碧波山庄>北叶青;茶园土壤总体上,pH值较适中,有机质含量很缺乏,全N含量偏低,全P含量中等,全K含量较高,有效N含量很缺乏,有效P含量非常丰富,有效K含量中等,并据此提出了关于该地区3个典型茶园今后合理施肥的一些建议。 相似文献
6.
山东省成武县农业地质环境土壤地球化学调查是按浅层、深层土壤样品1点/4km2。测试N,P,K,Cu,Zn,B,Mo,Mn,F,As,Hg,Pb,Cr,Cd等14种指标。在统计这些指标的表层、深层土壤地球化学特征参数的基础上,对其与世界、全省同类参数的差异进行了分析,并分析了区内表层、深层土壤元素含量的相关性,认为该区表层土壤元素含量的显著特征是高F,Hg,Pb而低Mo;大部分元素在表层土壤中的含量继承了土壤母质的成分特征,但N,F,Hg,Pb等受人为活动和污染源的作用在表层土壤中明显富集。通过分析表层土壤营养元素有效量可知,P,K,Zn的有效量高;供肥能力强;而Mo,Cu,Mn明显偏低。利用易污染元素浅层土壤含量值,通过污染指数法,对全区土壤污染程度进行了评价;区内土壤无严重污染区存在,并且明显污染地段面积较小,呈零星分布,说明区内污染程度较轻。 相似文献
7.
通过对桓台县域内表层土壤开展1∶5万土地质量地球化学调查与评价工作,统计了表层土壤地球化学参数,厘定了桓台县土壤地球化学背景值,并与山东省、淄博市元素平均值进行对比,发现土壤元素中Se、有机质、N,Zn,P,Hg,Cd,V,F,I含量明显偏高于山东省土壤均值;土壤元素中Se,I,P,N,Hg,Cd含量明显偏高于淄博市土壤均值;Se元素高于淄博市土壤均值。对表层土壤进行聚类分析和因子分析,根据聚类分析分组结果和各因子得分空间分布特征情况,结合研究区内土壤类型、地形地貌、土地利用方式的不同,综合考虑影响元素含量的各种因素,将研究区表层土壤分为5个地球化学分区,各分区元素组合特征不同。研究结果表明:土壤元素分布特征主要受控于地质背景,人类活动对土壤元素含量产生一定程度的影响。 相似文献
8.
山东省曹县地区土壤地球化学调查是按浅层土壤样品1点/4 km~2,深层土壤样品1点/16 km~2。测试N,P,K,Cu,Zn,B,Mo,Mn,F,As,Hg,Pb,Cr,Cd等14种指标。在统计这些指标的表层、深层土壤地球化学特征参数的基础上,对其与世界、全省同类参数的差异进行了分析,并分析了区内表层、深层土壤元素含量的相关性,认为该区表层土壤元素含量的显著特征是高F而低P,Zn,Mo。大部分元素在表层土壤中的含量继承了土壤母质的成分特征,但N,P,F,Hg等受人为活动和污染源的作用在表层土壤中明显富集。 相似文献
9.
研究了淮北平原砂姜黑土地区生姜氮钾配施的增产效应和对土壤养分的影响。结果表 明:氮钾配施可以大幅度提高生姜的产量,施钾的增产幅度,柴姜为15.3%～58.4%,平均增产率 为35.8%;狮子头姜产量提高18.2%～46.9%,平均增产28.7%。增施氮钾肥可有效提高土壤有 机质、全N、有效P、速效K、缓效K、有效Ca和有效Mg含量,降低NO3-盐含量,促使土壤pH趋于 中性,对全P和碱解N含量影响较小。土壤N素和P素大量盈余,不施钾时土壤K亏损严重,施钾 处理土壤钾基本上处于盈余状态,有利于维持和提高土壤肥力。 相似文献
10.
通过对山东省巨野县土壤元素背景值状况的计算和研究,发现土壤中Ca,Cd,Hg,Mg,F等元素显著高于全省和全国背景值;Mo,Pb,Cu,Co等元素则低于全省和全国背景值;其中土壤Mo含量远低于全省和全国平均水平。土壤质地是决定区内土壤N,K,Mg等元素含量的关键;由黄河冲积物发育的土壤P含量普遍较高,TOC空间分布与N密切相关。城镇及工业区土壤中Hg和Pb的积累趋势明显。元素分级结果显示,区内土壤K和有机质比较丰富;N,P和有机质缺乏区占比分别为23.82%,15.39%和6.47%。微量元素中Ca,Mg,S,Cl等元素较为丰富;而Mo,Si,Se,Co,Zn,Cu,Fe,Mn等元素的缺乏状况最突出。土地质量地球化学评价分等结果显示,全区大部分土地质量优良,区内东北部和中西部地区土壤肥力较好,但有害元素含量偏高,西北部地区肥力较差导致土地质量等级偏低。全区土壤有机质含量不足以满足农业生产需要,加之局部土壤盐分偏高,对粮食作物生长不利。区内土壤环境质量水平总体较好,多数重金属元素分布受地质背景控制,但Hg和Pb污染位置与城镇及工业区分布明显存在一定关系,高值区多呈点状分布于人类活动强烈的地带,说明工业或生活排放对区内土壤中Hg,Pb的积累贡献较大。 相似文献
11.
通过测定雷州半岛南部845个耕地土壤样品pH、有机质、全氮、有效磷、速效钾、碱解氮的含量,采用层次分析法确定各肥力评价指标权重,应用模糊数学法对该区域耕地土壤肥力进行综合评价,并利用ArcGIS 9.2软件对土壤肥力空间变异进行分析.结果表明:雷州半岛南部土壤有机质、全氮、有效磷、速效钾、碱解氮平均值分别为26.18 g/kg、1.48 g/kg 、34.63 mg/kg、158.57 mg/kg、133.17 mg/kg;土壤速效磷的变异系数最高,为103.14%,属强变异性,有机质、速效钾、碱解氮、全氮的变异系数属中等变异性,pH值的变异系数最小.土壤肥力总体水平处于中等偏低;从空间分布来看,土壤肥力中部高,东北、西南部相对较低 相似文献
12.
Pedogeochemistry of China is controlled by such factors as biology, climate, parent material, topography and anthropogenesis,
and the different geochemical types are formed under the different conditions of soil formation which have different abundance
levels of elements. The relationship between concentration of elements and plant growth and human health depends upon available
forms of element in soils. While the factors affecting element availability are soil pH and Eh, tillage and fertilization
by man besides element forms in soils. On the basis of pedogeochemical types and distribution, rational plantation and application
of fertilizer to soils will be of great significance for sustainable development of agricultural production. 相似文献
13.
Ｓｏｉｌｉｓａｎｅｐｉｇｅｎｅｔｉｃｓｐｈｅｒｅｈａｖｉｎｇｔｈｅｄｅｎｓｅｓｔｂｉｏｌｏｇｉｃａｌｍａｓａｎｄｔｈｅｈｉｇｈｅｓｔｂｉｏｌｏｇｉｃａｌｅｎｅｒｇｙ,ｗｈｉｃｈｉｓａｂａｓｅｍｅｎｔｐｒｏｖｉｄｉｎｇｔｈｅｐｌａｎｔｗｉｔｈｗａｔｅ... 相似文献
14.
On the basis of the soil environment investigation in Da'an City, Jilin Province, China, 40 soil samples from main land use types were obtained and tested by standard method. Soil organic matter (SOM), total N (TN), total P (TP), total K (TK), available N (AN), available P (AP) and available K (AK) were chosen as the evaluation factors. A regional soil nutrient evaluation model was developed based on the matter-element model. The results show that the soil samples with nutrient grade Ⅱ-Ⅴ respectively account for 10%, 30%, 32.5% and 27.5%, and those with grade Ⅳ and Ⅴ account for 60% in all samples. The relationship between soil nutrients and land types indicates that the nutrients of farmland are relatively good, with 41.7% of soil samples with the nutrient grade Ⅳ and Ⅴ. The nutrients of saline-alkali land and sandy land are the worst, with 100% of soil samples with the nutrient grade Ⅳ and Ⅴ. And the ratios of soil samples grade Ⅳ and Ⅴ in grassland and wasteland are respectively 62.5 % and 54.55%. Generally speaking, the soil nutrients status in Da'an City is poor, 60% of soil samples are in poor and extremely poor conditions, indicating that the soil has been severely eroded. Being a relatively superior evaluation method with more accurate resuits and spatial distribution consistency, matter-element analysis is more suitable for regional soil nutrient evaluation than previous models. 相似文献
15.
以茌平县土壤为研究对象,通过系统的地球化学调查,获取了土壤20余项指标含量数据;在此基础上计算了茌平县土壤中背景值和基准值等系列地球化学参数,圈定地球化学异常区,评价了土壤养分和环境地球化学等级、土壤质量地球化学综合等级。结果表明,与山东省土壤背景值平均值相比,茌平县土壤中K、Mn、Pb、V、Mo、I等元素偏低,而有机质、As、Cd、Hg、B等元素偏高。调查区7类异常区域均有分布;土壤质量综合评价以优质等级为主,约占全区面积的73.96%,良好等级约占全区面积的24.67%。 相似文献
16.
The relationship between forestland soil fertility and gathering firewood in the Zhuxi watershed in the red soil hilly region of China 总被引：1，自引：0，他引：1
Declining soil fertility has become an increasingly urgent problem and gathering firewood is one of the important contributing factors.Due to the excessive exploitation of natural resources especially for firewood,the red soil hilly region has become one of the most vulnerable eco-environment regions in China.The pressure of gathering firewood on forestland soil fertility in forestland has been generally estimated by geographical information system and questionnaire method in this paper in the Zhuxi watershed of Changting County,Fujian Province,China,a typical representative in the red soil hilly region of China.The results of this study show that:i) Forestland soil fertility is negatively affected by gathering firewood,which is more intensive in the integrated buffer zone than out of zone.The forestland soil fertility grade,OM,total N,available N,total P,available P,total K,available K,pH and <2μm clay content are lower and bulk density is higher in the integrated buffer zone than those out.ii) The forestland soil fertility grade,OM,total N,available N,total P,available P,total K,available K,pH and <2μm clay content tend to be lower and bulk density tends to be higher in the village buffer zones than those out in Datian,Chenguang and Youfang respectively.iii) The population density,economic development and terrain might be the key driving forces contributing to the relationship between gathering firewood and forestland soil fertility.Higher population density leads to more massive firewood collection and imposes more pressure on forestland soil fertility.Decreasing the use of firewood stove may reduce firewood consumption and thus release the pressure of gathering firewood on forestland soil fertility.Terrain affects the accessibility to gathering firewood thus affects forestland soil fertility.Other driving forces influencing the relationship between gathering firewood and forestland soil fertility should also be taken into account in the further study. 相似文献
17.
I INTRODUCTIONWetland has very important effect on retainingwater and against drought, regUlating climate, controlling soil erosion and so on ac. Today men often attachimportance to economic effect of wetland reclamation,but neglect and destroy other functions and effectswhich result in blind wetland development, a lot ofwetland degeneration. The area of freshwater wetland inthe 1950s was 134 x 10'ha, but in the 1970s 70% hadchanged into farmland (MITSCH, 1993). The area ofwetland in d… 相似文献
18.
Effects of Urbanization,Soil Property and Vegetation Configuration on Soil Infiltration of Urban Forest in Changchun,Northeast China 总被引：2，自引：0，他引：2
Peijiang Wang Haifeng Zheng Zhibin Ren Dan Zhang Chang Zhai Zhixia Mao Ze Tang Xingyuan He 《中国地理科学(英文版)》2018,28(3):482-494
Urban forest soil infiltration, affected by various factors, is closely related with surface runoff. This paper studied the effect of urban forest types, vegetation configuration and soil properties on soil infiltration. In our study, 191 typical plots were sampled in Changchun City, China to investigate the soil infiltration characteristics of urban forest and its influencing factors. Our results showed that the steady infiltration rates of urban forest soil were highly variable. High variations in the final infiltration rates were observed for different vegetation patterns and compaction degrees. Trees with shrubs and grasses had the highest infiltration rate and trees with bare land had the lowest infiltration rate. In addition, our results showed that the soil infiltration rate decreased with an increase in the bulk density and with a reduction in the soil organic matter content and non-capillary porosity. The soil infiltration rate also had significantly positive relationships with the total porosity and saturated soil water content. Urban soil compaction contributed to low soil infiltration rates. To increase the infiltration rate and water storage volume of urban forest soil, proper techniques to minimize and mitigate soil compaction should be used. These findings can provide useful information for urban planners about how to maximize the water volume of urban forest soil and decrease urban instantaneous flooding. 相似文献
19.
Soil organic carbon pool along different altitudinal level in the Sygera Mountains,Tibetan Plateau 总被引：1，自引：1，他引：0
Labile organic carbon (LOC) is one of the most important indicators of soil organic matter quality and dynamics elevation and plays important function in the Tibetan Plateau climate. However, it is unknown what the sources and causes of LOC contamination are. In this study, soil organic carbon (SOC), total nitrogen (TN), microbial biomass carbon (MBC), microbial biomass nitrogen (MBN) and LOC were analyzed based on different soil horizons and elevations using turnover time in an experimental site (3700 m to 4300 m area) in Sygera. SOC and LOC in higher-elevation vegetation types were higher than that of in lower-elevation vegetation types. Our results presented that the soil microbial biomass carbon (SMBC) and soil microbial biomass nitrogen (SMBN) were positively correlated with SOC. The content of easily oxidized carbon (EOC), particulate organic carbon (POC) and light fraction organic carbon (LFOC) decreased with depth increasing and the content were the lowest in the 60 cm to 100 cm depth. The total SOC, ROC and POC contents decreased with increasing soil horizons. The SOC, TN, MBC and MBN contents increased with increasing altitude in the Sygera Mountains. The MBC and MBN contents were different with the changes of SOC (p<0.05), meanwhile, both LFOC and POC were related to total SOC (p<0.05). The physical and chemical properties of soil, including temperature, humidity, and altitude, were involved in the regulation of SOC, TN, MBC, MBN and LFOC contents in the Sygera Mountains, Tibetan Plateau. 相似文献