三高农业与土肥

三高农业与土壤和肥料有密切的关系。地力是作物产量的重要基础,要取得高产,就必须坚持不懈地培肥地力。综合地力、土壤中营养元素及有害或有毒物质的含量、肥料类型和施肥技术,都对农产品的品质有很大的影响。要提高农产品的产量和质量,就要因土种植,合理施肥。高产优质是经济效益的主要构成因素,因而,培肥地力、因土种植、合理施肥能提高经济效益。忽视土肥工作,将影响三高农业的发展。     

不同轮作模式对潮土团聚体及其有机碳分布的影响

为揭示不同轮作模式下潮土土壤团聚体及其有机碳含量变化规律,于2018-2019年在山西大同进行了田间试验.设置处理为油菜—荞麦(RB)、玉米—荞麦(CB)、马铃薯—荞麦(PB)和燕麦—荞麦(OB)4种轮作模式,荞麦—荞麦(BB)连作和休闲—休闲(FF)为对照,测量指标为土壤团聚体组成、稳定性和团聚体内有机碳分布.结果显示:与连作模式(荞麦—荞麦)相比,各轮作模式均提高了土壤大团聚体数量和稳定性;油菜—荞麦(RB)轮作模式0-60 cm土层的大团聚体含量均增加,其0-20 cm土层的平均重量直径(MWD)、几何平均直径(GMD)增幅为5%和7%,20-40 cm土层的团聚体R0.25、MWD、GMD值增幅为8%、26%和37%.各轮作模式土壤有机碳主要富集在土壤表层,且>3 mm粒级土壤团聚体中有机碳含量对整个土壤有机碳含量和土壤有机碳库的贡献率最高.同时,各轮作模式0-20 cm土层各个粒级团聚体的有机碳含量均显著增加,油菜—荞麦(RB)轮作模式20-40 cm土层各个粒级团聚体的有机碳含量显著增加,随粒径级数递减其增幅分别为41%、49%、72%和39%,其>3 mm粒级团聚体的有机碳储量及贡献率也最高.总之,轮作有利于增加土壤团聚体的有机碳含量,可改善土壤团聚体组成及稳定性,增加土壤的固碳能力,但不同轮作模式间有差异.本研究表明油菜—荞麦轮作更有利于土壤固碳,可以在研究区域作为重要轮作模式进行推广和应用.(图2表5参41)     

CBM-CFS3: A model of carbon-dynamics in forestry and land-use change implementing IPCC standards

The scientific community, forest managers, environmental organizations, carbon-offset trading systems and policy-makers require tools to account for forest carbon stocks and carbon stock changes. In this paper we describe updates to the Carbon Budget Model of the Canadian Forest Sector (CBM-CFS3) implemented over the past years. This model of carbon-dynamics implements a Tier 3 approach of the Intergovernmental Panel on Climate Change (IPCC) Good Practice Guidance for reporting on carbon stocks and carbon stock changes resulting from Land Use, Land-use Change and Forestry (LULUCF). The CBM-CFS3 is a generic modelling framework that can be applied at the stand, landscape and national levels. The model provides a spatially referenced, hierarchical system for integrating datasets originating from different forest inventory and monitoring programs and includes a structure that allows for tracking of land areas by different land-use and land-use change classes. Ecosystem pools in CBM-CFS3 can be easily mapped to IPCC-defined pools and validated against field measurements. The model uses sophisticated algorithms for converting volume to biomass and explicitly simulates individual annual disturbance events (natural and anthropogenic). Several important scientific updates have been made to improve the representation of ecosystem structure and processes from previous versions of CBM-CFS. These include: (1) an expanded representation of dead organic matter and soil carbon, particularly standing dead trees, and a new algorithm for initializing these pools prior to simulation, (2) a change in the input data requirement for simulating growth from biomass to readily available merchantable volume curves, and new algorithms for converting volume to biomass, (3) improved prediction of belowground biomass, and (4) improved parameters for soil organic matter decay, fire, insect disturbances, and forest management. In addition, an operational-scale version of CBM-CFS3 is freely available and includes tools to import data in standard formats, including the output of several timber supply models that are commonly used in Canada. Although developed for Canadian forests, the flexible nature of the model has enabled it to be adapted for use in several other countries.     

设施土壤pH值与有机质演变特征研究

设施土壤的pH、有机质与土壤环境质量及设施栽培作物生产水平密切相关。文章对云南不同区域、不同大棚种植年限、不同轮作制度的设施土壤pH与有机质的演变特征进行研究,结果表明:大棚种植年限长的地区,土壤pH、有机质变化明显;随着大棚种植年限的增长,土壤pH呈下降趋势,有机质含量则呈上升趋势;随着土壤层次的加深,大棚土壤pH逐渐升高,而有机质则逐渐降低;不同轮作方式,花-菜轮作比菜-菜轮作有利于增加有机肥对设施土壤pH的缓冲性。     

耕作方式对土壤微生物和土壤肥力的影响

通过2年田间定位试验,对比研究了免耕+秸秆覆盖、旋耕+秸秆覆盖和传统耕作:三种耕作方式对土壤温度、土壤呼吸速率、土壤微生物数量和土壤肥力状况的影响.结果表明:秸秆覆盖对地温的影响存在"双重效应";土壤温度、土壤呼吸速率和土壤微生物量碳三者之间存在凸面关系;秸秆还田后耕作措施对土壤0～10和10～20 cm的微生物数量的影响不同,但均能增加土壤微生物量;土壤微生物能够加快秸秆中的有机碳向土壤有机质的转化速率;土壤微生物量碳可以作为反映土壤生产力状况的重要生物学指标之一.     

Integrated effects of slope aspect and land use on soil nutrients in a small catchment in a hilly loess area,China

This study addressed the integrated effect of slope aspect and land use on soil nutrients in a loess hilly catchment in the western Loess Plateau of China. Soil samples were collected from five land-use types: wasteland, cropland, woodland, shrubland and abandoned cropland, at two depths (0–20 and 20–40 cm) in the middle slope position of both north-facing and south-facing slopes. Soil nutrient changes and the relationships between soil nutrients and slope aspect were investigated, based on statistical analysis and expert knowledge. Soil organic matter, total N, total P, nitrate nitrogen and available K of the 0–20 cm soil layer differed significantly between land uses and slope aspects. Soil nutrients in the north-facing slope were better than in the south-facing slope. Revegetation has an enrichment effect, especially on soil organic matter, total N, total P, nitrate nitrogen and available K. Planting of trees, shrubs and grasses could improve soil fertility and favours a policy of revegetation and sustainable land use in the hilly loess area of China. Conversion of slope farmlands into more sustainable land uses, such as shrubland or grassland is a cost-efficient way to achieve soil conservation and ecological restoration. Terracing and the use of agro-techniques for soil conservation, such as furrow-ridging tillage and leaving crop residues on fields, can increase the input of C to soils. Growing crops in rotation with alfalfa and beans could be a promising choice for the sustainability of agriculture and the environment.     

Soil management for sustainable crop disease control: a review

Excessive use of agrochemicals in conventional crop management has caused serious environmental and health problems including loss of biodiversity and human disorders. A number of chemical biocides have shown complex chronic effects such as change in endocrine functions and immune systems. Application of different chemical biocides to the soil and plants have increased substantially over the last five decades. Total consumption of chemical fertilizers worldwide increased tenfold from 1950 to 2000. This is also true for chemical biocides with its annual current use of 3 billion l and a value of 30 billion dollars. There are ample evidences indicating that plants which grow in rich soil associated with N-P-K availability are prone to pests and diseases. Managing and exploiting soil environmental conditions as part of an integrated control strategy can make a significant contribution to agricultural sustainability and environmental quality. Application of organic matter and practises which increase the total microbial activity in the soil might enhance general suppression of pathogens by increasing competition for nutrients. Choice of crops in rotation with plants less susceptible to specific pathogens causes a decline in population due to natural mortality and the antagonistic activities of co-existent root zone microorganisms. Plants growing in disease-suppressive soil resist diseases much better than in soils with low biological diversity. Understanding the effect of soil environmental factors on plant disease incidence and the best crop management strategies to prevent, avoid, escape and control diseases were the aims of this literature review. This article comprises the main topics on soil fertility associated with N-P-K and other macro- and micro nutrients, and also soil pH, structure and texture, organic matter and microbial reserves, describes the use of various crop management practises which reduce the incidence of plant diseases.     

Effects of Recent Land-Use Practices on Soil Nutrients and Succession under Tropical Wet Forest in Costa Rica

The effects of a variety of agricultural land uses were studied using soil nutrients, forest structure, and species assemblages as indicators. We compared soil properties and successional forests between abandoned cacao ( Theobroma cacao ) and abandoned palm ( Bactris gasipaes ) orchards, abandoned pasture, and mature forest. These sites co-occupy an alluvial terrace soil ( Andic Dystropept ) at La Selva Biological Station, Costa Rica. The agricultural sites were originally cleared of most or all forest vegetation approximately 30 years ago and went into succession approximately 7 years ago. Forest structure, species composition, soil nitrogen and phosphorus pools, and nitrogen-mineralization and nitrification rates were measured for each site. The abandoned palm orchard had lower basal area and stem density than other secondary forests of the same age. It also had significantly smaller nitrate (NaOH-extractable) and organic phosphorus pools and significantly lower net rates of nitrogen-mineralization and nitrification. It is evident that preserving tree cover does not necessarily maintain soil fertility. We found species richness and diversity in the secondary forests to be positively correlated with basal area at the time of abandonment.     

Dynamics of soil organic matter in primary and secondary forest succession on sandy soils in The Netherlands: An application of the ROMUL model

We applied the simulation model ROMUL of soil organic matter dynamics in order to analyse and predict forest soil organic matter (SOM) changes following stand growth and also to identify gaps of data and modelling problems. SOM build-up was analysed (a) from bare sand to forest soil during a primary succession in Scots pine forest and (b) on mature forest soil under Douglas fir plantations as an example of secondary succession in The Netherlands. As some of the experimental data were unreliable we compiled a set of various scenarios with different soil moisture regime, initial SOM pools and amount and quality of above and below ground litter input. This allowed us to find the scenarios that reflect the SOM dynamics more realistically. In the Scots pine forest, total litter input was estimated as 0.50 kg m⁻² year⁻¹. Two scenarios were defined for the test runs: (a) forest floor moisture regimes—‘dry, mesic and hydric’ and (b) augmenting a root litter pool with three ratios of needles and branches to roots: 1:1, 1:1.5 and 1:2.0. The scenario finally compiled had the following characteristics: (a) climate for dry site with summer drought and high winter moisture of forest floor; (b) a litter input of 0.25 kg m⁻² year⁻¹ above ground and 0.50 kg m⁻² year⁻¹ below ground; (c) a low nitrogen and ash content in all litter fall fractions. The test runs for the estimation of the initial SOM pools and the amount and proportion of above and below ground litter fall were also performed in the Douglas fir plantation. The inputs of above ground litter tested in various combinations were 0.30 and 0.60 kg m⁻² year⁻¹, and below ground litter 0.30, 0.60 and 0.90 kg m⁻² year⁻¹. The scenario that fitted the experimental data had an SOM pool of 20–25 kg m⁻², an aboveground litter input of 0.6 kg m⁻² year⁻¹and a below ground litter input of 0.9 kg m⁻² year⁻¹. The long-term simulation corresponded well with the observed patterns of soil organic matter accumulation associated with the forest soil development in primary and secondary succession. During primary succession in Scots pine forest on dry sand there is a consistent accumulation of a raw humus forest floor. The soil dynamics in the Douglas fir plantation also coincide with the observed patterns of SOM changes during the secondary succession, with SOM decreasing significantly under young forest, and SOM being restored in the older stands.     

新垦赤红壤不同轮作的养分变化

五年的研究结果是:赤红壤耕垦之后只要采取合理的轮作和结合适当的秸秆返回措施,它的肥力就可以得到保持,而且还可以获得显著提高。在四种轮作形式中,效果最明显的为1:1,它的土壤有机质、全量N、P、K含量比轮作前分别提高了L 22、1.84、2.27和0.06倍1:2和2:1的效果较差,分别提高了0.57、0.83、2.08、0.39倍和1.02、0.91、1.46、-0.07倍,0:1的由于没有轮作,加上每年把长好的草皮铲走,导致了土壤有机质、全氮量反而比轮作前下降了6.5％和25.0％。随着轮作土壤养分的提高,土壤物理和微生物状况也获得了改善。     

整地施肥对尾叶桉生长及土壤性状的影响

整地施肥试验结果表明，全垦、带垦和穴垦三种整地方式以及施肥对尾叶按造林成活率和保存率均无明显的影响，成活率在９５％－９８．８％之间，保存率在９２．１％－９７．７％之间．整地能改变土壤性状，如土壤孔隙度全垦为５７．８８％。穴垦为４９．４２％；对林木生长有促进作用，但作用效果很快减少，如造林３年后的林木材积全垦、带垦分别为穴垦的１３６．４％和１２０．０％，５年后却分别下降到１１６．５％和１０８．３％．施肥可提高土壤养分，促进林木生长．造林５年后的调查结果，穴垦施肥林地的土壤有机质、速效Ｎ分别为１５．４４７ｇ／ｋｇ和４９．２３０ｍｇ／ｋｇ，林木年均树高生长为１．２５ｍ；不施肥处理的有机质、速效Ｎ分别为１０．３８８ｇ／ｋｇ和３５．７１５ｍｇ／ｋｇ，林木年平均生长量为０．３５ｍ；林木材积施肥处理的为不施肥的９．８倍．整地施肥还可提高林木叶片的养分含量．     

13C-dating, the first method to calculate the relative age of molecular substance homologues in soil

This article reports the design of ¹³C-dating, the first method to calculate the relative age of molecular substance homologues occurring in fractions from the same soil sample. Soil is a major carbon pool impacting modern climate by CO₂ release and uptake. Molecular substances that sequester carbon in soils are poorly known due to the absence of methods to study molecular-level C dynamics over agricultural time scales, e.g., 0–200 years. Here, I design a method to calculate the relative age of the plant-derived C₃₁ n-alkane occurring in 6 fractions from a soil sample naturally ¹³C-labelled by maize cropping during 23 years. Soil fractions are the bulk soil extract, two humin-encapsulated fractions and three particle-size fractions. Results show that C₃₁ n-alkane homologues have relative ages ranging from −6.7 years for the humin-encapsulated homologue to +25.1 years for the 200–2,000-μm fraction homologue. Such a wide variation of 31.8 years evidences temporal pools of molecular substances in soil. This finding also reveals that physical encapsulation can strikingly change the dynamics of a single molecular substance. ¹³C-dating thus allows to assess the carbon storage potential of molecular substances from crop soils. Such knowledge will help to identify molecular compounds, associated soil pools and agricultural practices that favour carbon sequestration. ¹³C-dating is further applicable to any environmental sample containing organic matter subjected to a ¹³C isotope shift with time. ¹³C-dating will also help to study the sequestration and delayed release of chemicals in various disciplines, such as pollutants in environmental sciences, pharmaceuticals in medicine, and nutrients in food science.     

Conversion from agriculture to grassland builds soil organic matter on decadal timescales.

Soil organic matter (SOM) often increases when agricultural fields are converted to perennial vegetation, yet decadal scale rates and the mechanisms that underlie SOM accumulation are not clear. We measured SOM accumulation and changes in soil properties on a replicated chronosequence of former agricultural fields in the midwestern United States that spanned 40 years after perennial-grassland establishment. Over this time period, soil organic carbon (SOC) in the top 10 cm of soil accumulated at a constant rate of 62.0 g x m(-2) x yr(-1), regardless of whether the vegetation type was dominated by C3 or C4 grasses. At this rate, SOC contents will be equivalent to unplowed native prairie sites within 55-75 years after cultivation ceased. Both labile (short turnover time) and recalcitrant (long turnover time) carbon pools increased linearly for 40 years, with recalcitrant pools increasing more rapidly than expected. This result was consistent across several different methods of measuring labile SOC. A model that investigates the mechanisms of SOM formation suggests that rapid formation of stable carbon resulted from biochemically resistant microbial products and plant material. Former agricultural soils of the Great Plains may function as carbon sinks for less than a century, although much of the carbon stored is stable.     

Spatial distribution and controlling factors of heavy metals contents in paddy soil and crop grains of rice–wheat cropping system along highway in East China

There is consensus concerning the heavy metal pollution from traffic emission on roadside agricultural land. However, few efforts have been paid on examining the contamination characteristics of heavy metals in roadside paddy-upland rotation field, and especially in combination with detailed quantitative analysis. In this study, we investigated the concentrations of heavy metals (Pb, Cd, Cr and Zn) in soil and crop grains of the rice-wheat cropping system along a major highway in East China in 2008 and analyzed the spatial distribution characteristics of heavy metals and their influencing factors with GIS and Classification and Regression Trees (CART). Significantly elevated levels of heavy metals in soil, rice and wheat grains indicated the heavy metals contamination of traffic emission in roadside rice-wheat rotation field. The contamination levels of Cd, Cr and Zn in wheat grain were higher than rice grain, while that of Pb showed an opposite trend. Obvious dissimilarities in the spatial distributions of heavy metals contents were found between in the soil, rice and wheat grains, indicating that the heavy metals contents in the roadside crop grains were not only determined by the concentrations of heavy metals in the paddy soil. Results of CART analysis showed that the spatial variation of the heavy metals contents in crop grains was mainly affected by the soil organic matter or soil pH, followed by the distance from highway and wind direction. Our findings have important implications for the environmental assessment and crop planning for food security along the highway.     

A simulation model to evaluate the impacts of invasive earthworms on soil carbon dynamics

Recent studies have reported that earthworm invasions alter native communities and impact nutrient cycling in terrestrial ecosystems. We developed a simulation model to evaluate the potential impacts of earthworm invasions on carbon dynamics, taking into consideration earthworm feeding strategies and priming effects on the microorganisms through their casting activities. Responses of carbon stocks (forest litter, soil organic matter, microbial biomass and earthworm populations) and carbon fluxes (litter decomposition, earthworm consumption, and microbial respiration) were used to evaluate an earthworm invasion of a forest ecosystem. Data from a northern temperate forest (Arnot Forest, New York) were adapted for model calibration and evaluation. Simulation results suggest that the impact and outcome of earthworm invasions are affected by pre-invasion resource availability (litter and soil organic matter), invasive earthworm assemblages (particularly feeding strategy), and invasion history (associated with earthworm population dynamics). The abovementioned factors may also determine invasion progress of earthworm species. The accuracy of the model could be improved by the addition of environmental modules (e.g., soil water regimes), precise parameters accounting for individual species attributes under different environmental conditions (e.g. utilization ability of different types of food resources), as well as earthworm population dynamics (size and structure) and interactions with predators and other invasive/indigenous species during the invasion progress. Such an earthworm invasion model could provide valuable evaluation of the complicated responses of carbon dynamics to earthworm invasions in a range of forest ecosystems, particularly under global change scenarios.     

不同施肥模式对华北平原小麦-玉米轮作体系产量及土壤硝态氮的影响

为了探索培育高产粮田的施肥模式,实现氮肥资源的高效利用与环境效益,以华北平原的小麦（Triticum aestivum）-玉米（Zea mays L.）轮作体系作为研究对象,通过2007─2011年4个轮作季,探讨不同的施肥模式对作物产量和土壤硝态氮的影响。试验以处理A（当地传统管理）作为对照,从测土确定施肥量、按作物生长发育明确施肥时期、合理分配各时期的养分配比及增施有机肥等方面改变传统施肥模式,设置3种高产施肥培育模式,分别为处理B（现有高产田推荐管理）、处理C（高肥料投入管理）和处理D（水肥高效管理）,进行田间小区试验。4个轮作季的总产量以处理D为最高,达75430 kg·hm-2,其次是处理C为75166 kg·hm-2,当地传统的产量最低。冬小麦季的吸氮量为处理C和D显著高于A处理,分别高出444.78 kg·hm-2和310.20 kg·hm-2,但与处理B无显著差异;处理D在夏玉米季的吸氮量为776.75 kg·hm-2,显著高于处理A。处理B的氮肥偏生产力值最高为38.21,处理D为36.71,处理A和C均为28.33。各处理经过4个轮作季后,土壤硝态氮均在120-160 cm出现累积峰,A、B、C和D的硝态氮峰值分别为58.65、28.98、105.89、45.29 mg·kg-1。在0-100cm土层,处理B的硝态氮累积量达到144.22 kg·hm-2,显著高于处理A、C、D;所有处理在100-200 cm土层均出现较高的硝态氮累积,处理C高达1021.19 kg·hm-2;0-400 cm的土壤硝态氮累积量分别为724.27、711-92、1324.30、730.70 kg·hm-2。处理A、B、C、D在耕层土壤氮素的表观损失分别为1298.95、653.18、1236.39和718.43 kg·hm-2,处理B、D显著低于处理A、C,D和B间差异不显著。因此,处理D是培育高产的理想施肥模式,合理的施肥量、科学的施肥时期以及有机无机的合理配比是达到高产、提高肥效和环境友好的关键。     

有机肥中重金属特征及其控制技术研究进展

随着工业的快速发展,农药、肥料及地膜等系列农用化学物质的广泛使用,农田土壤重金属污染越来越严重。重金属进入土壤后,其难移动性导致大量积累,造成土壤环境污染,影响植物生长,危及人类的健康。有机肥是我国农业生产中非常重要的肥料,其来源也十分广泛。施用有机肥是提高作物产量的必要措施,同时也是土壤重金属的主要输入途径之一,研究有机肥的重金属特征及其有关控制技术对农产品安全和有机废弃物的再利用具有重要意义。文章就畜禽排泄物堆肥、污泥堆肥、生活垃圾堆肥和沼肥等主要有机肥料的重金属来源、含量以及不同溯源有机肥料对土壤中重金属有效性的影响进行综述,重点介绍了畜禽排泄物堆肥中重金属含量和饲料添加剂之间的关系,为农田土壤重金属污染防治和农产品安全提供科学依据。除从有机肥的源头控制重金属外,文章主要介绍了化学法、生物吸附法、生物淋滤法和电化学法等重金属控制技术,针对各种控制方法,阐述了其原理、应用实例、优缺点及研究进展情况,提出了解决有机肥重金属污染问题的思路和方法,为有机肥料的资源化利用提供了参考。最后指出,为了实现养殖业与种植业的安全链接,除选用重金属含量低的有机肥,通过相关技术有效控制有机肥中的重金属外,还要注重肥料用量、施肥时间、施肥技术的合理选择,从最大程度上避免有机肥料给作物和人类带来的副作用。     

秸秆还田条件下农田系统碳循环研究进展

秸秆还田是农田生态系统的固碳减排的一种措施,现已成为国内外学者研究的热点。本文在分析农田系统碳循环流通的基础上,将系统划分为土壤、植物和大气3个子系统,对秸秆还田条件下各个子系统中碳的流动变化情况进行讨论。在土壤子系统中,秸秆还田对土壤有机碳（SOC）、土壤矿化碳、土壤微生物碳（MBC）的变化都有作用。秸秆还田的初期可能会降低微生物利用碳源的能力,影响群落物种分布的均匀度,致使作物对碳、氮利用率下降;然而,长期的效应仍会增加土壤微生物的多样性和活性。研究亦认为秸秆还田特别是与有机肥配合使用,能够提高土壤有机碳的含量;对土壤有机碳矿化具有明显促进作用,但是对土壤原有的有机碳矿化影响尚不清楚。秸秆还田在植物子系统中的影响主要集中在植物光合碳变化。已有的研究表明秸秆还田对作物光合作用的影响表现为正效应;然而根际碳流通的变化尚不清楚。在大气子系统中,秸秆还田能够增强旱地耕作土壤的呼吸作用,促进CO2的排放;而淹水条件下,秸秆还田使土壤有机碳矿化受到了明显抑制,对CO2没有明显影响。与此类似,淹水条件促进CH4排放,排水良好可以减少CH4的释放。事实上对CH4的排放而言,水份的影响可能比秸秆还田所产生的影响更大。笔者认为秸秆还田后土壤有机碳流通变化机理,及根际碳的流通变化影响仍有待进一步解析。其次,农业机械使用所产生的 CO2气体在研究秸秆还田模式时也应被考虑在内。除此之外,秸秆还田这种减排措施（CO2）的减排潜力、适宜应用的区域、可能的协同作用和一些限制及不利因素还没有得到确切的评估,实施过程中应考虑社会和经济层面上的因素。     

长期施肥对土壤有机质积累的影响

20年的NPK施肥定位试验,有利于深刻揭示土壤肥力特征与营养平衡规律。以位于黄淮海平原的中国科学院禹城综合试验站为例,探讨和估算了长期定量施肥对冬小麦（TriticuspaestvumL．）、夏玉米（ZeaMaysL．）生长和土壤有机质（SOM）的影响。结果表明,长期的N、P肥配施或N、P、K均衡施肥,可显著增加SOM储量,并且后者要优于前者;SOM增加主要集中在0-20cm深度的土层,40-60cm基本不变;生物量对SOM储量变化影响明显,NPK,NP处理作物生长良好,作物残体输人明显优于其他处理;0-40cm可以代表该区用以计算土壤固碳潜力,并且在N、P、K均衡施肥条件下,0-40cm土层中SOM储量长期以来持续增加,并未达到上限,每年的平均固碳速率（以C计）达182．8kg·hm-1,约是全球平均水平的1．5倍,全国平均水平的1．1倍。华北平原若按N、P、K均衡施肥,农田土壤每年固碳潜力将达到1．6-2．4Tg·a-1。     

施用污泥堆肥对作物和土壤的影响

污泥中的有机质、营养成分可为农业生产提供重要的有机肥源，但污泥中的重金属是制约污泥农用的重要因素，为检验污泥堆肥施用后对作物及土壤的影响，文章对污泥与稻草或木屑堆肥的产品进行了盆栽试验研究。结果表明，污泥与稻草或木屑的堆肥作为肥料施用于萝卜(Brassicacampestris)和菜心(Brassicaparachinensis),产量明显提高，部分堆肥产品增产效果优于化肥，且后效明显。堆肥施用使土壤中有机质、各养分含量增加，微生物活动增强、数量增加，然而作物和土壤中的重金属含量也有不同程度的提高。