Impact of slope farmland use change on ecosystem services value in China,2000-2020

Slope farmland is an important component of farmland resources in China.The utilization and change of slope farmland have significant effects on ecosystems,and understanding the impact of slope farmland change on ecosystem services(ESs)is critical for effective land utilization and ecosystem protection.This study aims to analyze slope farmland changes in China between 2000 and 2020 and quantify the impact of these changes on ESs by the use of a land use dynamic attitude study,and an ecosystem services value(ESV)equivalent.Results show that the area of slope farmland in China was mainly concentrated on slopes of 2°-6°,and exhibited a downward trend between 2000 and 2020.There were significant differences in the spatial distribution of the farmland,which was mainly located in the Taihang,Qinling,Wushan,and Xuefeng mountains.ESV increased by$179.235 million due to the conversion between slope farmland and forest,grassland,and construction land from 2000-2010.Conversely,from 2010 to 2020,ESV decreased by$2613.919 million due to the conversion of forest and grassland to slope farmland as well as the conversion of slope farmland to construction land.

Influence of Straw Incorporation on Maize Yield,N Accumulation and Remobilization on Slope Farmland in Northeast China

Slope farmland is a main type of agricultural land throughout northeast China.Long-term high intensity utilization and unreasonable farming have caused the deterioration of soil resources and a decrease in crop production.Here,it was hypothesized that crop straw incorporation might help to reduce nutrient losses and increase maize yields across time and space.A field experiment for testing straw management practices on maize across three slope positions(top,back and bottom slopes)was conducted in Northeast China in 2018 and 2019.In this study,the dry matter accumulation(DMA),N accumulation(NA),N remobilization,postsilking N uptake and grain yield were measured under SI(straw incorporation)and NSI(no straw incorporation)across three slope positions of 100-m-long consecutive black soil slope farmland during the maize(Zea mays L.)growth stages.Compared with NSI,SI significantly increased DMA and NA at the silking and maturity stages.SI typically increased the N remobilization in all slope positions,and significantly increased N remobilization efficiency and contribution of N remobilization to grain on the back and bottom slopes.However,post-silking N uptake was only increased by SI on the top slope.SI generally increased the crop yield in three slope positions.In the SI treatments,the bottom slope was the highest yield position,followed by the top,and then the back slopes,suggesting that the bottom slope position of regularly incorporated straw might have increased the potential for boosting maize yield.Overall,the study demonstrated the outsized potential of straw incorporation to enhance maize NA and then increase the grain yield in black soil slope farmland.

Extension Study on the Use of Slope Farmland in West Region

Based on the research of slope farmland in northern Shaanxi,the extension decision model was set up by the original theory of extenics. The optimal solution is obtained by expanding analysis,provide scientific basis for decision-making and increase the economic benefits to farmers.

Analysis of Comprehensive Benefits of Transforming Slope Farmland to Terraces on the Loess Plateau:A Case Study of the Yangou Watershed in Northern Shaanxi Province,China

De-farming slope farmland has been an effective measure in recent years to improve environment and prevent soil and water loss on the Loess Plateau.There are different views about the defarming method,and also various de-farming patterns have been put into practice.This paper takes the Yangou Watershed in Shaanxi Province of China as a case for studying the comprehensive benefits of transforming slope farmland to terraces.Based on the day-by-day meteorological data of the Yan'an station in 2005 and the data of terrain features,soil and land use data of the Yangou Watershed,the impact of transforming slope farmland on terraces were simulated and analyzed in aspects of yield increase and water-soil conservation under different topographic conditions with the aid of software WIN-YIELD.Furthermore,an empirical analysis was applied to study the effects of transforming slope farmland to terraces in the Yangou Watershed.The results show that:(1) The bigger the topographic gradient is,the more remarkable benefits it has in yield increase and water-soil conservation.(2) Farmland with slope below 5° could be retained,but farmland with slope above 15° should be converted to forest or grassland as soon as possible.(3) Transforming slope farmland to terraces has the same remarkable effects as the current policy of "Relieving and de-farming" in improving agricultural production conditions,safeguarding food security,raising permanent vegetation coverage rate,and preventing soil and water loss.Besides,it is more cost-effective than the policy of "Relieving and de-farming".It's strongly suggested that the policy of transforming slope farmland to terraces be carried out on the Loess Plateau without delay.

Spatial Disparity of Slope Farmland and Food Security in Three Gorges Area

As an important measure of eco-environmental construction, the process ofde-farming in slope farmland is being undertakengradually in the whole China. Meanwhile, theproblem of reducing in food yield in de-farming areas can not be neglected any more. It is especially the case in areas with concentrated slope farmland andinconvenient transportation. In this paper, we analyze the causes of hidden troubles in food security, and the spatial relationship between farmland and slopefarmland in the reservoir area of Three Gorges, and unveil the spatial disparity of contradictions between food supply and demand. Finally, combining the accessibility of areas, three different spatial types offood security, food security area, food alert area, and food crisis area, are divided.

Environmental emigration stress of slope farmland in the Three Gorges area

The project of ‘grain for green’, to restore woodland and grass by retreating from slope farmland, as a fundamental measure of eco-environmental rehabilitation, is being conducted in the reservoir area of the Three Gorges gradually. However, the de-farming of slope farmland will reduce the amount of farmland in de-farmed areas, especially in the areas with concentrated slope farmland, which would cause the problems of environmental emigration. The people who cannot regain enough farmland by relocating farmlands within village after de-farming and have to emigrate to other places are called environmental emigrants or ecological emigrants. In the research, a de-farming stress index model and an environmental emigration model are developed based on GRID data, and the potential amount of environmental emigration caused by de-farming of slope farmland in the reservoir area is simulated aided with GIS. The simulation indicates that the potential emigration amount caused by de-farming is quite large. When the de-farming stress index reaches 40%, the amount is as large as 890,000 people, which is equivalent to the emigrants caused by the submergence of the Three Gorges reservoir. So it should be considered as a big problem during the eco-environmental rehabilitation in this area. Some suggestions are raised to tackle the problem. Firstly, the emigration plan should be included in the de-farming plan. Secondly, some provinces, especially those located in the lower reaches of the Yangtze River, should accommodate part of the environmental emigrants.

Soil Erodibility of Slope Farmland in Guizhou Mountain Areas

This paper studied soil erodibility of slope farmland in Guizhou mountain areas by the plot runoff method,analysis and test. Results show that the variation coefficient of erodibility K value calculated according to formula introduced by Sharply is low and relatively stable and accurate,so it is a suitable method for calculating erodibility K value of slope farmland in Guizhou mountain areas. K value of layer A slope farmland decreases with increase of years. The erodibility of entire soil layer is high,and the erosion resistance is weak. From the influence of different planting system and use types in 4 years,K values of different soil layers decrease,average reduction of A,B and C layers reaches 3. 17%- 11. 64%( 1. 26%- 12. 34% for layer A,1. 29%- 13. 80% for layer B,and 1. 26%- 10. 80% for layer C). Except engineering terraced treatment,the decline of K value of grassland,zoning crop rotation,economic fruit forest,grain and grass intercropping,plant hedge, and mixed forest treatment is higher than farmers' treatment,and the decline level is grassland > zoning crop rotation > economic fruit forest > grain and grass intercropping > plant hedge > and mixed forest treatment. Planting grass and trees is favorable for lowering erodibility of slope farmland and improving farmland quality. Interplanting of corns with other plants can increase plant coverage and species,so it is favorable for improving erodibility of slope farmland.

Characteristics of Soil Respiration of Terraces and Slope Farmland in Loess Hilly and Gully Regions

Soil CO_2 emissions of terraces and slope farmland in loess hilly and gully regions were measured by using Infra Red Gas Analysis(IRGA),and the diurnal variation characteristics of soil respiration rate in different slope positions of terraces and slope farmland were analyzed.The results show that the diurnal variation curves of soil respiration rate of terraces and slope farmland in loess hilly and gully regions had a single peak.The soil respiration rate of terraces reached the peak during 13:00-15:00,while the soil respiration rate of slope farmland reached the peak from 11:00 to13:00,and it was the lowest at next 07:00.The daily average of soil respiration rate in slope farmland was 0.86μmol/(m^2·s),accounting for 93.48% of that of terraces.The daily average of soil respiration rate in different slope positions of terraces and slope farmland is shown as follows:the bottom of the slope>the middle of the slope>the top of the slope.At the top of the slope,the daily averages of soil respiration rate in terraces and slope farmland were the same;at the middle and bottom of the slope,the daily average of soil respiration rate in terraces was larger than that of slope farmland.

Eco-environment Restoration and Regional Differentiation Characteristics Based on “Building Terrace and Returning Slope Farmland to Forests and Grass”

Based on the scientific and technological achievements in the past decade in the Loess Hilly-gully Region and the successful demonstration experience in Yan'an Yangou watershed, we summarize the characteristics of eco-environment restoration pattern based on "building terrace and returning slope farmland to forests and grass". According to the data on land use, slope farmland and the agricultural population in 1999, we calculate the area of new terrace that needs to be built, the area of garden plot that needs to be extended, vegetation restoration area and investment demand in counties (cities, districts). Establishing and using some indicators, such as basic farmland extension indicator, garden plot extension indicator, vegetation restoration index and investment demand density, we conduct type classification and analysis of regional differentiation characteristics in 55 counties (cities, districts). The results show that in the Loess Hilly-gully Region, 691 600 hm2 of new terrace needs to be built, 792 000 hm2 of economic forests and orchards need to be extended, 5 410 200 hm2 of vegetation needs to be restored, and the total investment demand is 15.82 billion yuan; in terms of geographical distribution, obviously there are two key areas for eco-environment restoration (one is located in the border area between northern Shaanxi and northwestern Shanxi, and the other is located in the eastern Gansu and southern Ningxia area); the classified regional guidance policies should be formulated as soon as possible, and the limited funds should be concentrated in the key areas.

农田排水沟除草护坡及生态净化研究综述

对农田排水沟除草护坡及生态净化等方面的研究进行了综述,并对目前主要使用的除草技术,生态护坡技术,以及发展前沿的生态净化技术等方面的国内外相关成果进行总结归纳。然而这些方法都存在技术单一、影响环境等缺点,在对各影响因素的协同作用进行综合系统分析的基础上,提出新的解决思路。对沟道运行面临的问题与需解决的科学问题进行了探讨,旨在为现代农业灌溉排水区域建设提供参考。

不同作物种植模式下坡耕地产流产沙的模拟研究

产流产沙是坡耕地水土流失的主要形式,为探讨不同种植模式对坡耕地产流产沙的影响,采用室内人工模拟降雨试验方法,在同一坡度、3种雨强下对坡耕地7种种植模式进行模拟试验。结果表明:1)不同种植模式下坡面产流量随雨强增大而增大,初始产流时间随雨强增大而缩短。坡面产流量趋势为先逐渐增大,之后(10 min左右)逐渐趋于稳定。C单种模式减流效果最差;A-B-C套种模式减流效果最好;低矮作物单种及参与的套种模式能更好促进降雨入渗。2)不同种植模式下坡面产沙量与雨强呈正相关,低矮作物参与的种植模式径流含沙量变化幅度较小,中、高单种或套种模式径流含沙量变化复杂。小、中雨强下,A-B-C套种模式减沙效果最好;大雨强下,A-B套种模式减沙效果最好。低矮作物参与的种植模式减沙效果优于中、高作物单种其套种模式。3)不同种植模式下产流量和雨强均呈极显著正相关。B、C单种模式与A-B-C套种模式产沙量与雨强有相关关系,其余模式与雨强的相关性不显著。综上,低矮作物单种及低矮作物参与的套种模式能有效减流、保土,因此坡耕地在进行农作物种植时应考虑增加低矮作物参与种植,避免造成大量水土流失。

三峡库区山区乡村功能多元化与坡耕地演变的耦合关系

探究快速城市化、工业化背景下,山区乡村功能多元化与坡耕地演变的耦合关系,对山区耕地保护和乡村可持续发展具有重要意义。从人地关系视角,构建了山区乡村功能多元化与坡耕地演变耦合关系测度模型,并以三峡库区奉节县为例,采用乡村功能评价、耦合协调度模型等方法,揭示其耦合关系及其驱动机制。结果表明:(1)奉节县各乡村功能均呈现发展的趋势,其中社会保障功能的发展最为明显,乡村功能综合指数呈现南北部增加、中部减少的特征,且南部增加幅度大于北部;(2)奉节县坡耕地占比呈现下降趋势,缓坡耕地减少最少,急陡坡耕地减少最多,呈现南部减少幅度小、北部减少幅度大的特征;(3)乡村功能多元化与缓坡耕地演变的耦合协调度呈下降的趋势,与陡坡耕地和急陡坡耕地的耦合协调度呈先降后升的趋势,其耦合响应类型可以归纳为可持续型、转型型、一致型和衰退型4种类型;(4)乡村功能多元化与坡耕地演变耦合变化主要受到自然、社会经济、政策等要素驱动,今后应当从发展生态农业、推行环境治理等方面来提高乡村功能发展与坡耕地利用之间的协调性。研究方法和研究结果可为其他山区坡耕地资源的优化利用、生态保护以及乡村可持续发展提供借鉴价值。

黑土区坡耕地水土保持耕作措施对土壤理化性状的影响

为探寻黑土区坡耕地不同水土保持耕作措施对土壤理化性状的影响机理,开展了田间小区试验。设置横坡耕作(TP)、垄向区田(RF)、深松(SF)、横坡耕作+垄向区田(TP-R)、横坡耕作+深松(TP-S)、垄向区田+深松(RF-S)3种水土保持耕作措施及3种组合耕作措施,并以常规顺坡耕作(CK)为对照,分析了土壤孔隙度、土壤机械组成、水稳性土壤团聚体稳定性、土壤养分含量等指标,并采用TOPSIS模型对不同水土保持耕作措施进行了综合评价,筛选了土壤稳定性强且蓄水保肥效果良好的水土保持耕作措施。结果表明:在玉米的全生育期内,深松、垄向区田、横坡耕作均能提高土壤体积含水率。TP-S处理体积含水率最大,0~40 cm土层平均体积含水率较CK处理增加29.47%;RF-S处理平均孔隙度最大,TP-S处理次之,平均孔隙度较CK处理分别增大10.68%、9.25%;TP-S处理能够显著提高土壤稳定性,其中平均质量直径(MWD)、几何平均直径(GMD)和大团聚体含量(R0.25)较CK处理分别增加12.30%、19.57%、13.97%;TP-S处理能够改善土壤机械组成,TP-S处理粗砂粒、粉粒、黏粒含量较CK处理增加15.40%、26.89%、1.90%,细砂粒含量较CK处理降低31.56%;TP-S处理IN(无机态氮)、AP(有效磷)、AK(速效钾)含量最高,较CK处理IN、AP、AK含量分别增加42.81%~55.32%、39.69%~40.68%、20.41%~25.45%。由TOPSIS模型综合评价结果可知,TP-S处理贴合度最高,土壤结构更稳定,且蓄水保肥效果更好,为适宜该地区的水土保持耕作措施。

玉米间作大豆行比配置对坡耕地水土流失的影响

[目的]探究玉米间作大豆不同行比配置的水土流失规律,为坡耕地具有水土保持效果的玉米间作大豆模式推广利用提供科学依据。[方法]在坡耕地条件下以玉米间作大豆为研究对象,选定坡度(10°,16°,22°)和降雨强度(40,80,120 mm/h),通过人工模拟降雨试验,探究玉米、大豆单作及玉米‖大豆2∶1(2行玉米间作1行大豆),2∶2,2∶3,2∶4行比配置的水土流失特征。[结果]玉米‖大豆2∶4行比配置较玉米单作、玉米‖大豆2∶1,2∶2,2∶3行比配置、大豆单作地表径流量平均减少64.23%,57.19%,31.17%,10.12%,0.36%,侵蚀量平均减少82.90%,80.75%,46.53%,29.78%,36.33%,地表径流产流时间平均延缓101.55%,49.06%,23.13%,30.77%,0.82%。雨强和径流产生时间、入渗流产生时间呈极显著负相关,和径流量、侵蚀量呈极显著正相关,坡度和径流产生时间呈显著负相关,在高雨强、高坡度下间作较大豆单作水土保持效果表现更好。[结论]总体来看,玉米‖大豆2∶4行比配置在不同雨强和坡度下水土保持效果较好,是一种合理可行的山区坡耕地作物多样性种植方式。

东北典型黑土坡耕地不同坡位土壤团聚体特征分析

“漫川漫岗”是东北黑土区典型地貌,其典型黑土土壤结构受径流、冻融等作用影响。为探明东北黑土坡耕地土壤团聚体分布特征,选取坡耕地的坡下、坡中、坡上位置采集土壤样品,测定不同坡位下水稳性团聚体粒径分布、稳定性指标及土壤性质,分析水稳性大团聚体与土壤pH、有机质、钙镁比关系及稳定性指标与团聚体粒径关系。结果表明,不同坡位下水稳性团聚体粒径分布均表现为<0.25 mm团聚体含量占比最高,>2 mm团聚体含量占比最少。<0.25 mm团聚体表现为坡下位显著高于坡中位及坡上位(P<0.05),0.25~0.5 mm、0.5~1 mm、1~2 mm、>2 mm团聚体均表现为坡上位显著高于坡下位(P<0.05)。平均重量直径和几何平均直径均表现为坡上>坡中>坡下,其中坡下位与坡上位、坡中位存在显著差异(P<0.05),团聚体水稳性表现为坡上>坡中>坡下。平均重量直径、几何平均直径均表现为与>0.25 mm团聚体呈正相关,与<0.25 mm团聚体呈负相关,其中受>2 mm团聚体影响最大(P<0.01)。有机质、pH、钙镁比均与>0.25 mm团聚体呈正相关关系(P<0.05)。因此,典型黑土坡耕地较高的有机质含量、pH、钙镁比有利于土壤团聚,促进>0.25 mm团聚体形成,提高团聚体水稳性。

典型黑土区坡耕地表层土壤活性有机碳变化特征

以典型黑土区3种地貌类型区(漫川漫岗区、丘陵漫岗区、平原低地区)坡耕地不同坡位表层土壤为研究对象,通过测定土壤总有机碳、高活性有机碳、中活性有机碳和低活性有机碳等指标,分析黑土区坡耕地不同坡位表层土壤活性有机碳的变化特征,探究不同地貌类型区坡耕地土壤活性有机碳变化特征的差异。结果表明,坡耕地各坡位表层土壤总有机碳含量变化范围为26.57~38.61 g/kg,土壤活性有机碳含量变化范围为1.85~5.67 g/kg。3种地貌类型区坡耕地不同坡位土壤总有机碳和活性有机碳含量变化特征不同。漫川漫岗区总有机碳、中活性有机碳和低活性有机碳含量变化特征均表现为坡上和坡中显著大于坡下、坡上和坡中无显著差异;高活性有机碳含量变化特征则以坡中最高坡下最低,且不同坡位之间高活性有机碳含量差异显著。丘陵漫岗区不同坡位土壤总有机碳和低活性有机碳含量差异显著,并表现为坡下显著大于坡上、坡上显著大于坡中;高活性有机碳和中活性有机碳含量的变化则呈现坡上和坡下显著大于坡中、坡上和坡下无显著差异。平原低地区总有机碳及3种活性有机碳组分的含量在各坡位间的差异均为未达显著水平。不同地貌间典型黑土区坡耕地表层土壤活性有机碳分布规律有所差异,漫川漫岗区和丘陵漫岗区坡耕地土壤有机碳活性最差的坡位分别是坡下和坡中,而平原低地区不同坡位间无显著变化。研究结果为黑土坡耕地生态建设与保护技术的针对性设计奠定了理论基础。

等高反坡阶措施下坡耕地球囊霉素相关土壤蛋白对土壤碳氮储量的贡献

为证实坡面微地形改造措施—等高反坡阶(CRT)对坡耕地的生态修复功能,揭示CRT对球囊霉素相关土壤蛋白(GRSP)含量及土壤碳氮储量贡献的影响与机制至关重要。通过分析原状(CK)和CRT处理下旱季和雨季坡耕地0—5、5—15、15—30 cm土层中总GRSP(T-GRSP)、易提取GRSP(EE-GRSP)、土壤有机碳(SOC)与土壤全氮(TN)在CRT阶上和阶下及CK对应位置处的时空分布特征,探讨CRT措施下GRSP对土壤碳氮储量的贡献,揭示相关机制。结果表明:(1)CRT坡耕地土壤T-GRSP、EE-GRSP、SOC和TN的含量较CK显著提高(P<0.05),增幅分别为16.6%—189%、7.28%—102%、1%—68.3%和7.29%—79.7%。且CRT对坡耕地GRSP含量的提升效果总体表现为雨季强于旱季、表层(0—5 cm)土壤高于深层(15—30 cm)、阶下优于阶上。(2)相比CK,CRT坡耕地旱季和雨季SOC储量分别提高8.06%和13.5%,TN储量提高7.01%和12.1%。T-GRSP对SOC和TN储量的贡献率较CK分别提高8.5%—141%和2.58%—133%,EE-GRSP对SOC和TN储量的贡献率较CK分别提高1.38%—82%和5.25%—87.2%。且CRT对坡耕地SOC和TN储量提升效果雨季优于旱季,对表层土壤T-GRSP对SOC和TN贡献率的提升效果表现为雨季强于旱季、阶下强于阶上。(3)CRT极大提高了坡耕地T-GRSP与土壤孔隙度、SOC和TN的正相关性。相比CK,相关系数(R~2)分别由0.17、0.26和0.29增至0.51、0.66和0.64。因此,CRT措施不仅降低了坡耕地SOC和TN的流失,还通过提高有机质含量改善土壤通气透水性,进而提高坡耕地GRSP的分泌与累积,同时提高GRSP对碳氮的贡献率,促进了土壤碳氮的固持与封存。

基于梯度提升树模型的坡耕地土壤水蚀模拟与分析

[目的]针对黄土高原坡耕地土壤侵蚀过程复杂、人为干扰强烈且难以量化的特点,利用机器学习定量解析主要影响因素对坡耕地土壤水蚀的作用与贡献,模拟分析坡耕地土壤水蚀特征并探究其机理,为坡耕地土壤侵蚀的预报提供基础支撑。[方法]基于黄土高原子洲试验站坡耕地小区1959—1969年产流产沙观测数据,精细化表征其影响因子,运用梯度提升树模型对侵蚀量和径流深的变化及其影响因素的贡献进行分析。[结果]数据集中次降雨侵蚀量(0~122.72 t/km^(2))、径流深(0.02~17.20 mm)、降雨历时(2~1410 min)及平均雨强(0.02~4.63 mm)属强变异,变异系数均>1,且多数变量呈右偏态;在相同训练集和测试集划分情况下,对侵蚀量模型预测精度(R^(2)=0.81)略优于径流深模型(R^(2)=0.80),但侵蚀量模型的层数(8层)大于径流深模型(5层),表明侵蚀机理相较径流机理更为复杂;通过梯度提升树模型与SHAP算法对自变量重要性进行排序发现,影响侵蚀模型与径流模型的自变量重要性不同。[结论]受特征提取的限制,在侵蚀量与径流深较小时预测结果不理想,未来研究应当通过引入更多自变量组合方式寻找更多相关变量以提高对侵蚀事件的预测。产流和产沙的主要影响因素存在差异,降水本身特征对产流过程起主要作用,侵蚀产沙过程中主要受到降水与地形相关自变量的共同影响。基于数据驱动,为揭示黄土高原坡耕地侵蚀机理提供参考,并为区域坡耕地土壤侵蚀防治提供科学依据。

坡耕地红壤剖面磷的储存容量及其流失风险研究

基于土壤磷储存容量的变化差异,准确评估与判断坡耕旱地与稻田红壤磷的剖面流失风险。以江西鹰潭孙家典型红壤小流域内位于坡上(T)、坡中(M)及坡下(B)的花生旱地(PU)及稻田(PF)各发生层土壤为对象,分析了各发生层土壤全磷(TP)、有效磷(Olsen-P)、磷饱和率(PSR)、磷吸持指数(phosphorussorptionindex,PSI)及磷储存容量(Soil phosphorus storage capacity,SPSC)随剖面的变化特征及差异,估测了坡耕地红壤磷的剖面流失风险,探讨了土壤pH、Eh及容重(BD)等因子对坡耕地红壤发生层SPSC的影响差异。结果表明,不同坡位花生旱地与稻田红壤表层TP、Olsen-P含量均显著高于底层土壤,且稻田红壤TP与Olsen-P的剖面变异显著高于花生旱地剖面。与耕作层(Ap1)相比,花生旱地底层土壤PSI显著增加了33.1%~146%,且随剖面深度增加而缓慢降低;而稻田红壤PSI则随着剖面深度增加而增大。花生旱地与稻田红壤(PF-M除外)PSR均随着剖面深度的增加而逐渐降低,SPSC变化范围分别为–89.2~298.3 mg·kg^(-1)与^(-1)38.1~101.1mg·kg^(-1)。PU-T与PU-M剖面SPSC均为正值,且随剖面深度增加呈降低趋势;而PU-B(耕作亚层Ap2除外)剖面的SPSC均为负值。PF-T(氧化还原层Br2除外)、PF-M(Ap1除外)及PF-B剖面各发生层的SPSC均为负值,且随剖面深度增加变化显著。基于SPSC理论对坡耕红壤剖面土壤磷储量及其环境流失风险的评估,花生旱地土壤磷沿剖面及坡位的迁移与运移迹象明显,当土壤Olsen-P>27.6mg·kg^(-1)时,花生旱地剖面土壤磷的流失风险将急剧增加,应及时采取管控措施。稻田红壤剖面各发生层均存在不同程度的磷流失风险,需立即停止施磷并及时采取有效措施。

三峡库区乡村坡耕地长时间序列动态演变与转型

研究山区坡耕地动态演变与利用转型,对中国西南山区传统乡村的粮食安全和农业可持续发展具有一定指导意义。以三峡库区腹地草堂溪流域为研究对象,利用ArcGIS 10.2软件并结合Fragstats、土地利用转移矩阵等技术手段对坡耕地的演变和驱动机制进行分析。结果表明:(1)坡耕地面积持续减少,与1965年相比,2020年坡耕地面积减少8004.7 hm^(2),整体动态度达7.21%,随着社会经济的发展坡耕地动态演变更趋活跃;坡耕地面积随高程级、坡度级的增加而先增后减,随聚落距离的增加而迅速减少。(2)坡耕地LPI、MPS、AI呈减小的趋势,MNN不断增加;坡耕地规模减小、破碎化程度加剧,斑块连片集中化程度减弱。(3)坡耕地主要向果园、林地和草地等转换,坡耕地生产功能主要转换为生态经济功能和生态功能,部分转换为生活功能。(4)山区坡耕地动态演变和利用转型可以归纳为生态经济型、撂荒型和生态型3种模式,其演变主要受到自然、社会经济、政策等多种因素的共同作用。研究结果揭示了50多年来三峡库区坡耕地的动态演变及转型特征,对库区山区农村土地利用、乡村可持续发展以及人地关系的改善具有启示意义。