• <tr id="yyy80"></tr>
  • <sup id="yyy80"></sup>
  • <tfoot id="yyy80"><noscript id="yyy80"></noscript></tfoot>
  • 99热精品在线国产_美女午夜性视频免费_国产精品国产高清国产av_av欧美777_自拍偷自拍亚洲精品老妇_亚洲熟女精品中文字幕_www日本黄色视频网_国产精品野战在线观看 ?

    Understanding the effects of contour hedgerow and terracing hedgerow on soil and water conservation in the remote mountainous regions of Southwest China

    2017-06-06 12:00:33ZHOUPingWENAnbangYANDongchunSHIZhonglinLONGYi
    中國(guó)水土保持科學(xué) 2017年2期
    關(guān)鍵詞:坡耕地西南地區(qū)水土保持

    ZHOU Ping, WEN Anbang, YAN Dongchun, SHI Zhonglin, LONG Yi

    (Institute of Mountain Hazards and Environment, Chinese Academy of Sciences and Ministry of Water Resources, the Key Laboratory of Mountain Surface Processes and Ecological Regulation, 610041, Chengdu, Sichuan, China)

    Understanding the effects of contour hedgerow and terracing hedgerow on soil and water conservation in the remote mountainous regions of Southwest China

    ZHOU Ping, WEN Anbang?, YAN Dongchun, SHI Zhonglin, LONG Yi

    (Institute of Mountain Hazards and Environment, Chinese Academy of Sciences and Ministry of Water Resources, the Key Laboratory of Mountain Surface Processes and Ecological Regulation, 610041, Chengdu, Sichuan, China)

    [Background] Soil and water loss is a serious worldwide environmental problem, for example, soil loss from the sloping cultivated lands in the remote mountainous regions of Southwest China due to the abundant precipitation and steep sloping cultivated lands in these areas. Various soil protection techniques have been adopted to prevent soil loess, the local people did not admire the introduced contour hedgerow measurement from abroad; however, they have been actively accepted another traditional one, the terracing hedgerow. The purpose of this work is to understand the differences on soil and water conservation between contour hedgerow and terracing hedgerow. [Methods] The different structure between four treatments of contour hedgerow and terracing hedgerow were analysed. Meanwhile, three heights (0 cm, 10 cm, and 15 cm) of lynchet were set, and the soil erosion module, runoff efficiency, ratio of output and input, economic effects among the different treatments were compared. The soil anti-scourability was calculated using the equation, and analysis of variance (ANOVA) was performed with SPSS 11.5 and Microsoft Excel software. [Results] The obvious difference was that terracing hedgerow with a certain height of walkway was more convenient for farming activities and effectively reduced soil and water loss. The treatment of terracing hedgerow 2 (H15H) reduced runoff 55.56%±6.25% and reduced erosion modulus 79.26%±3.50% when compared to the sloping cultivated land plots with no lynchet and no hedgerow (CK). The contributions of the independent variables on runoff, soil erosion reduction and soil anti-scouring were in the following order: terracing hedgerow 2 (H15H) > terracing hedgerow 1 (H10H) > contour hedgerow (H0H) > non-hedgerow (CK). The value of ratio of output to input of H15H treatment was 1.52, which was the highest value among different treatments. [Conclusions] Although the treatment of terracing hedgerow 2 (H15H) needs more labour force, however, results in the higher hedgerow yield and ratio of output to input than other treatments as well as stronger anti-scourability. Thus, the traditional terracing hedgerow with 15 cm lynchet is recommended in the remote mountainous regions of Southwest China, even should be recommended often and used extensively in the similar climatic regions in other countries.

    terracing hedgerow; structure; mechanism of the soil and water conservation; contour hedgerow

    0 Introduction

    Soil and water loss is a serious environmental issue worldwide. In China, nearly one third of the lands suffered from soil and water loss[1]. Especially serious soil and water loss problems occur in the remote mountainous regions of upper Yangtze River region of China mainly due to abundant precipitation and the characters of the soils. Additionally, soil erosion is the main cause of the loss of nutrient-rich topsoil and the declination of soil fertility, and thus is a potential threat to safety of the Three Gorges Dam. Soil degradation by erosion affects 1966 million hectares worldwide[2]. The total soil erosion in this region was about 11.98*107t/km2·a and the average modulus of soil erosion was 2.09 t/km2·a, depending on slope gradient and precipitation characteristics. Meanwhile, most of the population living in this region depends on agriculture for their livelihood; hence it is imperative to preserve soil to sustain crop yields in the Southwest China.

    The gully mountains are the main landscapes in the remote mountainous regions of Southwest China, with the high tillage index, overgrazing problem, severe soil erosion and fragile ecology. According to the results of agricultural and water conservation investigations, the main sediment source of Yangtze River was from the sloping cultivated land[3]. The broken terrain, complex geological construction, erosive topographic conditions, frequent landslide, debris flow hazards, serious soil loss, and water pollution have been the severe problems in this region, accelerating soil erosion on sloping lands[4], therefore, the soil erosion becomes a serious challenge for agricultural development in this region. On one hand, the sediments from the sloping cultivated land were the main sediment source of the rivers and lakes, and about 60%-78% of sediments of Yangtze River were from the sloping cultivated land[3]. On the other hand, the single land use pattern of sloping cultivated land, lower carry capacity, serious soil and fertilizer loss all lead to the thinner soil layer and lower land production. Also the vicious cycle of sloping cultivated land tillage - soil and water loss - production degraded - not meet people’s needs - reclaim the sloping cultivated land, which is the obstacle of the sustainable agriculture development of gully mountainous region of the Three Gorges Reservoir region at the upper reaches of Yangtze River[5].

    The total area of the Three Gorges Reservoir region is 5.24*104km2with the complex topography and the hilly mountainous area is 94.1%, the percentage of sloping cultivated lands is 41.54% of the total cultivated lands, and mainly distributed in the inconvenient irrigation and steep slope degree mountain regions. And the percentage of sloping cultivated lands with more than 25 slope degree is 28%[6]. Meanwhile, the sloping cultivated lands had the more serious soil erosion with the total soil erosion yield of 9.45*107t/a[7], also the land productivity decreased and faced to the ecological environment restoration and the sustained economic development[8]. Agroforestry can greatly reduce some losses, especially on hill slopes, where soil evaporation, runoff and soil losses are important. The agroforestry ecosystem such as the contour hedgerow was first introduced to sloping farmlands as an effective soil-conservation strategy in this region. However, it didn’t play a significant role in reducing soil erosion, controlling non-point source pollution and increasing economic effects. Also the local people realized that the agroforestry ecosystem such as the contour hedgerow caused some problems. Meanwhile, the local people also think that there exist traditional hedges and the plants grow well on the hedgerow, why do not we adopt this traditional mode (terracing hedgerow) and why we abandoned this traditional soil and water conservation strategy and adopted the introduced new soil and water conservation (contour hedgerow) from abroad? The local people’s attitudes and suggestion let us reconsider the traditional strategy of soil and water conservation. Meanwhile, most researchers noted that hedgerows were effective in controlling soil erosion, but very few explained the structures and mechanism behind that effectiveness. Also the relationship of spatial and temporal of the terracing hedgerow and the long time location tests were all needed by the ecological theories and ecological landscape theories.

    The objectives of this study are as follows: 1. comparing the conceptional differences between the contour hedgerow and the terracing hedgerow; 2. comparing the effects of soil and water conservation between the contour hedgerow and the terracing hedgerow.

    1 Materials and methods

    1.1 The concept of contour hedgerow

    The concept of contour hedgerow is to use the narrow vegetative strips of trees, shrubs or grasses planted on the contour, often called ‘contour hedgerows’, is an experimental management practice with potential to reduce soil erosion on sloping lands in the humid tropics[9]. Food crops are planted in the alleys where the areas are between the hedgerows (Fig. 1). It is one of effective soil conservation strategies recommended for tropical and subtropical mountainous regions. The contour hedgerow effectively reduced soil loss, runoff and associated nutrient losses on sloping terrain[10].The contour hedgerow was used very widely in the agricultural lands and forestlands in the foreign countries[11-12]. From the 1970s, the contour hedgerow as one important way of agroforestry ecosystem was favored by the tropical and subtropical regions such as the South Africa, India and Philippines. In China, only some places implemented the contour hedgerow, but it was not popularized by the local farmers.

    Fig.1 Composition and structure of a contour hedgerow

    1.2 The concept of terracing hedgerow

    The composition of terracing hedgerow includes the lynchet and the edge-of-field berms and the hedgerow (Fig.2). The “Lynchet” is an archeological term referring to the morphological response on a hill slope to the presence of field boundaries in filed berm. These edge-of-field berms may affect the rate and the distribution of runoff from the fields, as they may create temporary impoundments. If the soil is moving away from the boundary, soil loss occurs, otherwise accumulation occurs. The hedgerow may be planted on the lynchet, which has the effects to reinforce the lynchet and the edge-of-field berms to further control the soil and water loss on the sloping cultivated lands.

    Fig.2 Composition and structure of a terracing hedgerow

    1.3 The studied area

    Experiments were conducted at the soil and water conservation station in Zhongxian county (30°24′53″N, 108°10′25″E), Chongqing municipality city, which is located in the Three Gorges Reservoir region of the upper reach of Yangtze River in the Southwest China. The experimental station belongs to the Institute of Mountain Hazard and Environment, Chinese Academic of Sciences. With the mean annual rainfall of 1 150 mm, about 70% falls is from April to October. Soil is mainly purple soil (Orthic Entisols in the Chinese soil taxonomic system, Regosols in FAO taxonomy or Entisols in USDA taxonomy)[13]of fast weathering products of the Jurassic rocks of the Shaximiao Group (J2s). The character of purple soil in this area is shown in Tab.1.

    1.4 Experimental design and methods

    The experiment included 4 treatments with 3 replicates of each. The plots were designed as 3 m width, 15 m length down slopes. The experimental hedgerow was a kind of grazing grass (Cichoriumintybus) with the slope gradient of the plots all 15° (Tab. 2). The lynchet heights of the terracing hedgerow were set 0 cm, 10 cm, 15 cm and double rows of the grazing hedgerow were planted (0.1 m inter-row and 0.2 m among the row spacing). The hedgerow distance was 4.5 m between each plot. The details of experimental treatments and farming practice in the experimental plots are shown in Tab.3.

    Tab.1 Characters of purple soil at the soil and water conservation station in the Three Gorges Reservoir

    Tab.2 Designed treatments in the experimental plots

    Tab.3 Details of experimental treatments and farming practice in the experimental plots

    The initial soil water content and the bulk density were measured before the experiment. The runoff and soil erosion were monitored after a big precipitation with 96.4 mm during a whole day. Soil loss and runoff were collected after each natural rainfall event using collecting tanks with a volume of 1 m3. These tanks were connected indirectly to the erosion plots via one of 9 outlets of a divisor box placed between erosion plot and tank. The amount of runoff water and the soil loss were collected from collecting channels at the lower end of each plot and weighed. Meanwhile, crops and stover were harvested from each plot respectively. Then the grains and stover were oven dried at 70 ℃ until constant weight reached.

    The represented sites were selected for soil sampling. The soils were collected using soil hand auger (diameter 5 cm) at 10 cm soil depth intervals. The sampling soil depth ranged from 0 to 0.6 m. Three duplicates for each sampling site were taken to evaluate the enrichment ratio of the runoff sediments. The soil samples were air-dried, gently grounded with a mortar and pestle, homogenized, and divided into two parts. One part of the soil samples was sieved to pass through a 2 mm mesh for analyzing the particle size distribution. After the removal of organic matter with hydrogen peroxide, the particle fractions were determined in duplicate with the laser diffraction technique, i.e., using the MS2000 Laser particle size analyzer (Malvern Instruments, Malvern, England) to analyze the content of clay, silt and sandy. Another part of the soil samples was sieved to pass through a 0.25 mm mesh for analyzing the soil chemical character.

    1.5 Calculation and statistical analysis

    For each hedgerow mode, the soil anti-scourability was calculated using the equation:

    M=Q/(G1-G2)

    WhereMis the modulus of the anti-scouring (L/g),Qis the water weight during the scouring experiment, andG1,G2are the weights of the soil before and after scouring experiments.

    All results are recorded as means ± standard deviations. Analysis of variance (ANOVA) was performed with SPSS 11.5 and Microsoft Excel software. The significance level was set asP<0.05.

    2 Results

    2.1 Compositions and structures of the contour hedgerow and the terracing hedgerow

    The hill slopes with gradients less than 25° are more commonly used for farming in the Three Gorges Reservoirs region of the upper reach of Yangtze River. The terracing hedgerows are used commonly in this region. The composition and structures of the terracing hedgerow and the contour hedgerow were shown in Fig. 1 and Fig. 2. The configuration mode and the spatial distribution of the contour hedgerow and terracing hedgerow were different as the geographical condition and the local peoples’ demands[14]. The single and double rows of hedgerows with the same hedgerow type or the different hedgerow types are very common.

    2.2 The function of the terracing hedgerow

    The roots of the terracing hedgerow better enhanced the soil physical and chemical characters, increased the soil infiltration and the soil porosity capillary, also reduced the bulk density and the soil texture[15], and therefore enhanced the soil conservation and the potential soil productivity.

    The hedgerow was periodically mowed to 0.5 m height each time by two or three months. And the mowed stems and leaves were returned to the sloping cultivated land to increase the soil organic matter and soil fertilizers[16]. Many studies were carried out on the decomposition of the mowed hedgerows. Lupwayi[17]used the exponential model to simulate the decomposition process of the organic matter ofLeucaenaleucocephala. Bross et al[18]compared the influence of decomposition of coverage of branches and leaves of locust and clover underground and aboveground condition, and analyzed the decomposition effects of the lignin of locust and clover.

    As growingly horizontal terraces were constructed in the Three Gorges Reservoir region of the upper Yangtze River, the areas of the terrace reached 12% of the whole areas of the sloping cultivated lands. New lynchets of the terraces reached 3.2*104hm2each year. More and more people paid attention to the concret function of the lynchets and the edge of field berms. The roots of the terracing hedgerow enhanced the stability of the lynchets and the edge-of-field berms, also prolonged the longevity of the lynchet and field berms. Hedgerow also played an obvious part in reducing the soil loss and soil erosion modulus. There were three functional approaches to influence the moving process of sediment and weaken soil erosion from the sloping cultivated lands. Firstly, the precipitation was intercepted and the energy of rain drops was reduced by the hedgerows. Also the soil scourability of the sloping cultivated land was reduced by the aboveground of the hedgerow. Secondly, the function of the hedgerow roots in the soil further increased the soil infiltration and reinforced the lynchets, and the edge-of-field berms enhanced the anti-scourability of the soils. The results of Wu’s[19]showed that the soil anti-scourability reduced by the roots of the hedgerow was nearly equal to that by the whole plant. The runoff and sediment yield time of the sloping cultivated lands were delayed and shortened by the roots of the hedgerows. The third function was that the aboveground of the terracing hedgerow had the direct function to intercept the runoff and sediment, prolonged the infiltration time and reduced the soil fertilizer loss. All these three functions together reduced the soil and water conservation and enhanced the soil fertilizer of the sloping cultivated lands.

    The hydraulic characters of the runoff of terracing hedgerow were changed. The velocity of the runoff reduced in the upper position of the terracing hedgerow and the sediment taken by the runoff reduced, which led to the sediment deposit in these places. However, the velocity of the runoff increased in the lower position of the terracing hedgerow, and the sediment taken by the runoff also increased, which led to the aggravation of the sediment erosion in these places. All the two processes of the upper position and lower position of the terracing hedgerow reduced the slope gradient and terracing the sloping cultivated lands. Shen et al[20]showed that the hedgerow reduced the slope degree from 30°-34° to 15°-18° in 9 years. And the soil organic matter also increased from 0.9% to 1.61%. The hedgerows all grew on the lynchets and the edge-of-field berms of the sloping cultivated lands formed the alley for farmer to walk while doing some farming activities. It reduced the trample of the cropping lands and reduced the touch of field crops to influence the field yields. Finally, economic factors play a role in determining whether farmers will adopt or not such technology. The hedgerow systems had the disadvantage of providing only limited early returns on investment[21]. Farmers repeatedly complain about the fact that improved yield response only comes in several years after hedgerow establishment[22].

    2.3 Comparing the effects between contour hedgerow and terracing hedgerow

    2.3.1 Effects of soil and water conservation between the contour hedgerow and the terracing hedgerow

    The measured soil erosion modulus, runoff and runoff coefficient of the different strategies are shown in Fig. 3. The CK consistently had the highest runoffs, followed by the H0H,then was H10H. The H15H had the lowest runoff. The H15H reduced runoff 55.56%±6.25% when compared to CK, and it reduced runoff 21.11%±1.36% when compared to the H10H. In addition, the H15H reduced erosion modulus 79.26%±3.50% when compared to the CK, and it reduced erosion modulus 58.64%±5.87% when compared to the H10H. The H10H reduced soil erosion modulus by 49.85%±5.50% and the H10H reduced runoff by 43.66%±4.45% when compared to the CK. According to ANOVA, the differences in runoffs of the different treatments were not significant for the H0H (F=2.36,P=0.15), H10H (F=1.85,P=0.21) and H15H (F=1.63,P=0.27). Difference in soil erosion moduli of the different treatments were not significant for the HOH (F=1.36,P=0.16), H10H (F=1.55,P=0.21), but was significant for the H15H (F=1.73,P=0.05). The results showed that the H15H had better soil and water conservation effects than the other two types of hedgerow. And the terracing hedgerow showed more effects on control soil erosion of the sloping cultivated lands than reducing the runoff.

    Different letters on the data dots in figure caption are statistically significant (P<0.05).Fig.3 Characters of soil erosion modulus, runoff, and runoff coefficient among the different lynchet heights of terracing hedgerow and the contour hedgerow on the sloping cultivated plots

    2.3.2 Economic effects between the contour hedgerow and the terracing hedgerow

    When compared the contour hedgerow and the terracing hedgerows with different lynchet height to CK, the contour hedgerow and the terracing hedgerow needed more labor force to sustain the normal farming activities (Tab.4), however, the less crop seeds, fertilizer and pesticides than the CK, only about 89%-93% of the latter. Although the input of the labor force was more in the mode of terracing hedgerow than that in the contour hedgerow, the output efficiency of the terracing hedgerow was higher than the latter (Tab.4), because the hedges such as the soybean, maize, peanut and so on were planted in the lynchet of the terracing hedgerow and intercepted the soil nutrients into the field lands.

    The ratio of the output to input of the CK was lower than the hedgerow mode. The contour hedgerow was of 96% when compared to the terracing hedgerow. The H15H had higher ratio of output to input than that of the H10H. As to avoide the competition of sunlight, water and fertilizer with the crops in the field, the hedgerows were cutting down to 0.5 m for two to three month (Tab.5). The cutting parts were returned to the cropping field and to the edge of lynchet to increase the soil nutrients. Also in some places, the farmers planted the valuable hedgerow such as the grazing grass, medical materials and the flowers or plants to increase the incomes. The hedgerow of these kinds had the higher economic effects (Tab.5). The farmers obtained the additional gains to enhance their incomes from different hedgerows.

    Tab.4 Output and input of the contour hedgerow and the terracing hedgerow

    Note: The data in the above Table showed as mean values ± standard deviation. Values followed by the same letters in the same column are not significantly different (P<0.05). The same below.

    Tab.5 Economic effects of different types of hedgerow

    Tab.6 Characters of soil anti-scourability and soil particle composition among different hedgerow modes

    Note: * refers toP<0.05, ** refers toP<0.01, *** refers toP<0.001

    The H15H had the highest anti-scourability when compared to the contour hedgerow and the traditional non-hedgerow. It enhanced 29.67% of the anti-scourability as compared with other hedgerow modes. Meanwhile, the content of sand reduced 4.41% and the content of silt and clay increased 2.9% and 12.26%, respectively. The soil aggregates became better and the hedgerow with the higher lynchet played more obvious part in soil and water conservation (Tab.6).

    3 Discussions

    Contour hedgerows, defined as dense, erect, vegetative barriers made of stiff-stemmed grass that slow-down runoff and reduce erosion[23-24], potentially reduce runoff and soil loss by up to 60% and 80%[25-26], respectively, by filtration, deposition, and infiltration[27-28]. Nevertheless, the effects of contour hedgerows reduced runoff a soil loss only 50.04%±5.12% and 70.01%±2.87% in the present study. The main reason was that the planting density of the contour hedgerow was less in this region than that in the foreign countries, also the degree of the sloping cultivated lands is steeper in this region. And the effects of the contour hedgerow depended mostly on slope gradient, runoff volume and flow rate, size and density of sediment particles, grass species, density, interval and width of grass strips, underlying soil properties, and rainfall intensity and duration[29-30]. In previous research tests, vetiver grass (Chrysopogonzizanioides), switchgrass (Panicumvirgatum), tall fescue (Festucaarundinacea), and achnathemps pendens (Achnatherumextremiorientale) were very effective in reducing soil and water loss[31-32]. Among these grasses, vetiver grass has often been suggested in the tropical and subtropical regions due to its unique characteristics, including fast growth, deep and penetrating root systems, and high tolerance to adverse conditions. However, vetiver is not favored by the farmers in the Three Gorges Reservoir region for its poor economic value. In this region, the grazing grass was more popularily planted. Thus, one kind of grazing grass (Cichoriumintybus) was chosen to analyze its ecological and economic effectiveness in this study.

    Due to high amount of precipitation, fragmentized sloping cultivated land and steep slope and severely soil erosion, annual averaged soil erosion amount was 19 364.71*104t/a, and the mean soil erosion modulus was 2 741.48 t/km2·a in the Three Gorges Reservoir region of the Southwest China[33]. Our results clearly supported the hypothesis that the lynchet of the terracing hedgerow had the positive effects on soil and water conservation, also was suitable for applying on the sloping cultivated lands in this region. In this study, the terracing hedgerow significantly reduced the erosion modulus and the runoff than the contour hedgerow and non-hedgerow. The lynchet height of 15 cm of the terracing hedgerow was recommended in this region.

    The lynchet of the terracing hedgerow also significantly reduced the soil and water loss from the sloping cultivated land and nutrients loss. The hedge planted on the lynchet effectively reduced the runoff velocity, increased the soil infiltration and soil capillary porosity to further reduce the loss of runoff. The similar results of the grass hedges and micro-basins on reducing soil and water loss were showed by the Xiao and alley cropping for managing soil erosion of hilly lands in the Philippines[28]. The results of Long[33]showed that the erosion modulus of contour hedgerow (Boehmerianivea) averaged 802.50 t/km2·a and the nearby sloping cultivated lands with on hedgerow reached 20 299.70 t/km2·a. The efficiency of the soil erosion reduction was 65.1%. As to the soil erosion, most of the sediments were intercepted by the stems and leaves of the hedge. For a longer time, the slope degree became gentle and the soil and water loss were effectively controlled.

    The distance of the hedgerow played important part in reducing the erosion. However, the present study was mainly concentrated on the qualitative analysis of the mechanism of the soil erosion and runoff reduction, and more researches need. The typical study results showed that there existed the exponent relationship between the hedgerow coverage and the concentration of the runoff in the mode of the contour hedgerow. Nevertheless, it was nearly no research on the lynchet height of the terracing hedgerow. The study on the hedgerow showed the diversified trends, and the related basic theory should be strengthened[34].

    4 Conclusions

    The structures and the mechanism of soil and water conservation of the contour hedgerow and terracing hedgerow were studied in subtropical regions of Southwest China. The conclusions are as following:

    1) The obvious difference existed between the terracing hedgerow with a certain height of lynchet and the contour hedgerow. And the function of the lynchet was for farmers to walk on it in conducting the farming activities at more convenience, and effectively reduced the soil and water loss.

    2) The comparative results showed that the traditional non-hedgerow CK control plots consistently had the highest runoff, followed by the H0H (Contour hedgerow), and then was H10H (Terracing hedgerow 1 with 10 cm lynchet). The H15H (Terracing hedgerow 2 with 15 cm lynchet) had the lowest runoff. The H15H reduced runoff 55.56%±6.25%, reduced runoff coefficient 21.11% ±1.36% and reduced erosion modulus 79.26%±3.50% when compared to CK. These results indicated that the terracing hedgerow with 15 cm lynchet presented better soil and water conservation effects than the other two kinds of hedgerow in the Three Gorges Reservoir region.

    3) The contributions of the independent variables to runoff were in the following order: H15H>H10H>CK>H0H. Similarly, the contributions to soil loss and the soil anti-scouring were in the following order: H15H > H10H > H0H > CK. Therefore, these traditional terracing hedgerow practices should be recommended often and used extensively in similar climatic regions.

    4) Although the input of the labor force was more in the mode of terracing hedgerow than that in the contour hedgerow, the output efficiency of the terracing hedgerow was higher than the latter. Meanwhile, the farmers planted the high valuable hedgerows such as the grazing grass, medical materials and the flowers or plants to increase their incomes in some places of Southwest China.

    Acknowledgements

    The authors wish to thank the Foundation of STS Program of the CAS (KFJ-SW-STS-175) and the National Natural Science Foundation of China (41671286). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript. Also we would like to thank the anonymous reviewers and editors for constructive comments and English corrections on the manuscript.

    5 References

    [1] LI Z G, CAO W, LIU B Z, et al. Present status and dynamic variation of soil and water loss in China[J]. Soil and Water Conservation in China, 2008(12): 7.

    [2] LAL R. Soil erosion impact on agronomic productivity and environment quality[J]. Crit. Rev. Plant Science, 1998, 17(4): 319.

    [3] ZHANG X B, HE X B. Achievement of slope farm land regulation in upper Yangtze River[J]. Yangtze River, 2010, 41(13):21.

    [4] ZHANG P C, CHENG D B. Process and regulation of soil and water loss of slope farmland in South China[J]. Journal of Yangtze River Scientific Research Institute, 2017, 34(3):35.

    [5] LI S X, LIU S Z. Mode and effects of the watershed harness in the Yangtze River [J]. Soil and Water Conservation in China, 1999(9):42.

    [6] CHEN G J, XU Q, DU R H, et al. Study on the impacts and strategy of ecology and environment of the three gorges project[M]. Beijing: Science Press, 1995, 6:15.

    [7] WANG Y K, WEN A B, ZHANG X B. Study of soil erosion on cultivated slope land in severe soil loss regions of upper reaches of Yangtze River basin using137Cs technique[J]. Journal of Soil and Water Conservation, 2003, 17(2):77.

    [8] SHI D M, LU X P, LIU L Z. Study on functions of soil and water conservation by mulberry hedgerow intercropping of purple soil slopping farmland in Three Gorges Reservoir region[J]. Journal of Soil and Water Conservation, 2005, 19(3):75.

    [9] GILLEY J E, EGHBALL B, KRAMER L A, et al. Narrow grass hedge effects on runoff and soil loss[J]. Journal of Soil and Water Conservation, 2000, 55(2): 190.

    [10] BAUDRY J, BUNCE R G BUREL F. Hedgerows: an international perspective on their origin, function and management[J]. Journal of Environmental Management, 2000, 60(1):7.

    [11] Salvador B S, Cornu S, Cuoturier A, et al. Morphological and geochemical properties of soil accumulated in hedge-induced terraces in the Massif Central, France[J]. Soil & Tillage Research, 2006, 85(1): 62.

    [12] Cullum R F, Wilson G V, Mcgregor K C, et al. Runoff and soil-loss from ultra-narrow row cotton plots with and without stiff-grass hedges[J]. Soil & Tillage Research, 2007,93(1): 56.

    [13] HE X B, BAO Y H, NAN H W, et al. Tillage pedogenesis of purple soils in southwestern China[J]. Journal of Mountain Science, 2009,6(2):205.

    [14] ZHANG Y Q, QI S. Study on terrace bio-embankment in China: present situation and trend[J]. World Forestry Research, 2002, 15(3): 49.

    [15] CHEN Z J, LIAO X Y,LIU S Q. Improvement of slope cropland productivity, by applying agricultural technique of plant hedge-rows[J]. Journal of Soil and Water Conservation, 2003, 17(4):125.

    [16] LI Y B, XIE D T, YANG C X. The technique of planting living hedgerow in exploiting and utilizing slope lands[J]. Tropical Geography, 2001, 21(2): 121.

    [17] LUPWAYI N Z, HAQUE I. Leucaena hedgerow intercropping and cattle manure application in the Ethiopian highlands III. Nutrient balances[J]. Biology and Fertility of Soils, 1999, 28(2): 204.

    [18] BROSS E L, GOLD M A, NGUYEN P V. Quality and decomposition of black locust and alfalfa mulch for temperate alley cropping systems[J]. Agro-forestry Systems, 1995, 29 (3):255.

    [19] WU Q X, LI Y. A study on soil anti-scourability increased by root system of plant in the loess plateau: an experimental study on top soil anti-scourability increased by root system of herbs[J]. Journal of Soil and Water Conservation, 1990, 4(1):11.

    [20] SHEN Y C. Study on soil and water conservation benefit of agricultural technology of hedgerows in the Three Gorges areas[J]. Journal of Soil Erosion and Soil and Water Conservation, 1998,4 (2):61.

    [21] BAYARD B, JOLLY C M, SHANNON D A. The economics of adoption and management of alley cropping in Haiti[J]. Journal of Environment Management, 2007, 84(1): 62.

    [22] KIEPE P. Cover and barrier effect of Cassia siamea hedgerows on soil conservation in semi-arid Kenya[J]. Soil Technology, 1996,9:161.

    [23] KEMPER D, DABNEY S, KRAMER L, et al. Hedging against erosion[J]. Journal of Soil and Water Conservation, 1992, 47(4): 284.

    [24] DORIOZ J M, WANG D, POULENARD J, et al. The effect of grass buffer strips on phosphorus dynamics-a critical review and synthesis as a basis for application in agricultural landscapes in France[J]. Agriculture, Ecosystems and Environment, 2006, 117(1): 4.

    [25] KOELSCH R K, LORIMOR J C, MANKIN K R. Vegetative treatment systems for management of open lot runoff: review of literature[J]. Applied Engineering in Agriculture, 2006, 22(22): 141.

    [26] BHATTARAI R, KALITA P K, PATEL M K. Nutrient transport through a vegetative filter strip with subsurface drainage[J]. Journal of Environmental Management, 2009, 90(5): 1868.

    [27] WU J J, HUANG C W, TENG W J, et al. Grass hedges to reduce overland flow and soil erosion[J]. Agronomy for Sustainable Development, 2010, 30(2): 481.

    [28] XIAO B, WANG Q H, WANG H F, et al. Protective function of narrow grass hedges on soil and water loss on sloping croplands in northern China[J]. Agriculture, Ecosystems and Environment, 2010, 139(4): 653.

    [29] ROBINSON C A, GHAFFARZADEH M, CRUSE R M. Vegetative filter strip effects on sediment concentration in cropland runoff[J]. Journal of Soil and Water Conservation, 1996, 51(3): 227.

    [30] DELETIC A, 2001. Modeling of water and sediment transport over grassed areas[J]. Journal of Hydrology, 2001,248(1): 168.

    [31] BABALOLA O, OSHUNSANYA S O, ARE K. Effects of vetiver grass (Vetiveria nigritana) strips, vetiver grass mulch and an organo-mineral fertilizer on soil, water and nutrient losses and maize (Zea mays L.) yields[J]. Soil and Tillage Research, 2007, 96(1): 6.

    [32] PANSAK W, HILGER T H, DERCON G, et al. Changes in the relationship between soil erosion and N loss pathways after establishing soil conservation systems in uplands of Northeast Thailand[J]. Agriculture, Ecosystems and Environment, 2008, 128(3): 167.

    [33] LONG T Y, QIAO D, AN Q, et al. Estimating soil erosion in Three Gorges Reservoir area based on GIS and RUSLE[J]. Journal of irrigation and drainage, 2012, 31(2):33.

    [34] PU Y L, XIE D T, DI E J. Review on benefits and evaluation of hedgerow technique in slope land[J]. Soils,2012, 44(3): 374.

    2016-08-19

    2017-04-14

    S152.2

    A

    2096-2673(2017)02-0025-06

    西南山區(qū)等高植物籬和植物固結(jié)地埂的水土保持功能的理解

    周萍, 文安邦, 嚴(yán)冬春, 史忠林, 龍翼

    (中國(guó)科學(xué)院水利部成都山地災(zāi)害與環(huán)境研究所,山地表生過(guò)程與生態(tài)調(diào)控重點(diǎn)實(shí)驗(yàn)室, 610041, 成都)

    水土流失是個(gè)世界范圍的嚴(yán)重環(huán)境問(wèn)題,比如由于豐沛的降雨和陡坡耕作,造成的中國(guó)西南部偏僻山區(qū)的坡耕地水土流失。這些區(qū)域采取了多種保持土壤措施減少土壤流失,可當(dāng)?shù)剞r(nóng)民并不接受引進(jìn)的等高植物籬措施;而植物固結(jié)地埂是一項(xiàng)傳統(tǒng)的且當(dāng)?shù)剞r(nóng)民樂(lè)意接受的水土保持措施。本文比較了等高植物籬和植物固結(jié)地埂的結(jié)構(gòu),設(shè)置3種植物固結(jié)地埂高度0 (CK)、10 cm (H10H)、 和15 cm (H15H), 分析了等高植物籬(H0H)和上述3種地埂高度的植物固結(jié)地埂對(duì)徑流、侵蝕量的影響及產(chǎn)投比和經(jīng)濟(jì)效益,旨在理解當(dāng)?shù)剞r(nóng)民的選擇。研究結(jié)果顯示最明顯的區(qū)別是植物固結(jié)地埂具有一定高度的地埂能夠方便農(nóng)事活動(dòng)并且有效減少水土流失。植物固結(jié)地埂的第2個(gè)處理(H15H)比無(wú)地埂無(wú)植物籬的坡耕地處理(CK)減少?gòu)搅?5.56%±6.25% ,減少侵蝕量79.26%±3.50%。不同處理的徑流量、土壤侵蝕減少量和土壤抗蝕性變化順序?yàn)椋?H15H > H10H > H0H > CK。H15H的產(chǎn)投比最高為1.52.與其他試驗(yàn)處理相比,雖然H15H措施需要的勞動(dòng)力更多,但它具有較高的植物籬收獲量和產(chǎn)投比以及較強(qiáng)的抗沖蝕性。因此,西南地區(qū)坡耕地上推薦具有15 cm地埂高度的植物固結(jié)地埂措施(H15H) ,甚至該項(xiàng)水土保持措施可適用于與西南地區(qū)氣候相似的其它區(qū)域或是其它國(guó)家。

    植物固結(jié)地??; 結(jié)構(gòu); 水土保持機(jī)理; 等高植物籬

    ZHOU Ping (1981-),female, associate professor. Main research interests: soil and water conservation. E-mail: zp09@imde.ac.cn

    ?Corresponding author: WEN Anbang (1964-), male, professor. Main research interests: soil erosion. E-mail: wabang@imde.ac.cn.

    10.16843/j.sswc.2017.02.004

    Funded: the STS Program of the CAS (KFJ-SW-STS-175); the National Natural Foundation (41671286); State’s Key Project of Research and Development Plan (2016YFC0402301); 973 Project (2015CB452704).

    猜你喜歡
    坡耕地西南地區(qū)水土保持
    基于MCI指數(shù)的西南地區(qū)近60年夏季干旱特征
    水土保持探新路 三十九年寫春秋
    西南地區(qū)干濕演變特征及其對(duì)ENSO事件的響應(yīng)
    《水土保持通報(bào)》征稿簡(jiǎn)則
    水土保持
    山西隊(duì)?wèi)蛳蛭髂系貐^(qū)的傳播
    中華戲曲(2019年2期)2019-02-06 06:54:16
    水土保持
    建平縣實(shí)施國(guó)家坡耕地治理項(xiàng)目成效及經(jīng)驗(yàn)
    Завершено строительство крупнейшего комплексного транспортного узла на юго
    --западе Китая
    中亞信息(2016年7期)2016-10-20 01:41:30
    資陽(yáng)市雁江區(qū):防治并重 建管結(jié)合 創(chuàng)建坡耕地水土流失綜合治理示范區(qū)
    90打野战视频偷拍视频| 亚洲av电影在线进入| www日本在线高清视频| 伊人亚洲综合成人网| 日韩欧美国产一区二区入口| 亚洲精品av麻豆狂野| 国产欧美日韩一区二区精品| 国产野战对白在线观看| 热99国产精品久久久久久7| 成人国语在线视频| 黄色视频,在线免费观看| 亚洲全国av大片| 国产成人影院久久av| 每晚都被弄得嗷嗷叫到高潮| 色视频在线一区二区三区| 午夜精品久久久久久毛片777| 麻豆乱淫一区二区| 亚洲国产精品一区二区三区在线| 欧美av亚洲av综合av国产av| 欧美久久黑人一区二区| 亚洲熟女精品中文字幕| 精品亚洲成国产av| 精品亚洲乱码少妇综合久久| 午夜福利视频在线观看免费| 女人精品久久久久毛片| 久久精品人人爽人人爽视色| 国产视频一区二区在线看| 亚洲国产精品一区三区| 国产欧美日韩综合在线一区二区| 青青草视频在线视频观看| 久久久久久免费高清国产稀缺| 精品国产乱码久久久久久小说| 91精品三级在线观看| 我要看黄色一级片免费的| 1024视频免费在线观看| 午夜福利视频在线观看免费| 两性午夜刺激爽爽歪歪视频在线观看 | tocl精华| 久久久久精品人妻al黑| 99热全是精品| 成人影院久久| 1024香蕉在线观看| 国产成人啪精品午夜网站| 国产91精品成人一区二区三区 | 日本精品一区二区三区蜜桃| 精品少妇黑人巨大在线播放| 在线亚洲精品国产二区图片欧美| 这个男人来自地球电影免费观看| 一区二区日韩欧美中文字幕| 日韩欧美国产一区二区入口| 久久久久视频综合| 国产成人影院久久av| av在线老鸭窝| 两性午夜刺激爽爽歪歪视频在线观看 | 久久ye,这里只有精品| 国产真人三级小视频在线观看| 国产亚洲精品一区二区www | 2018国产大陆天天弄谢| 热re99久久国产66热| 老汉色∧v一级毛片| 99久久国产精品久久久| 久久热在线av| a级片在线免费高清观看视频| 亚洲国产成人一精品久久久| 成年人午夜在线观看视频| 国产av国产精品国产| 午夜精品国产一区二区电影| 亚洲国产中文字幕在线视频| 国产精品偷伦视频观看了| 亚洲专区字幕在线| 国产男人的电影天堂91| 男女下面插进去视频免费观看| 久久狼人影院| 日韩 亚洲 欧美在线| 91老司机精品| 久久久久国产一级毛片高清牌| 中国美女看黄片| 19禁男女啪啪无遮挡网站| 黄色a级毛片大全视频| 精品久久久久久电影网| 国产av精品麻豆| 久久久水蜜桃国产精品网| 久久精品aⅴ一区二区三区四区| 成人av一区二区三区在线看 | 女人被躁到高潮嗷嗷叫费观| 午夜激情av网站| 韩国高清视频一区二区三区| av免费在线观看网站| 97人妻天天添夜夜摸| 母亲3免费完整高清在线观看| 蜜桃国产av成人99| 中文字幕精品免费在线观看视频| 黄色毛片三级朝国网站| 欧美中文综合在线视频| 国产欧美日韩一区二区精品| 91av网站免费观看| 中文字幕精品免费在线观看视频| 亚洲第一欧美日韩一区二区三区 | 俄罗斯特黄特色一大片| 在线观看人妻少妇| 亚洲专区国产一区二区| 国产精品一区二区在线不卡| 十八禁人妻一区二区| 女人久久www免费人成看片| 久热这里只有精品99| 99精国产麻豆久久婷婷| 我的亚洲天堂| 国产成人啪精品午夜网站| 蜜桃在线观看..| 午夜福利在线免费观看网站| 亚洲 国产 在线| 亚洲自偷自拍图片 自拍| 久久人人爽av亚洲精品天堂| 久久久久国产一级毛片高清牌| 美女高潮到喷水免费观看| 少妇 在线观看| 一级毛片女人18水好多| 久久久久视频综合| 久久九九热精品免费| 交换朋友夫妻互换小说| 国产免费av片在线观看野外av| 一区二区三区乱码不卡18| 丝袜美足系列| 欧美一级毛片孕妇| 精品国产乱码久久久久久小说| 一级片免费观看大全| 91成年电影在线观看| 国产精品国产av在线观看| 另类精品久久| 日本vs欧美在线观看视频| 中文字幕另类日韩欧美亚洲嫩草| 亚洲视频免费观看视频| 久久人人97超碰香蕉20202| 999久久久精品免费观看国产| 女人爽到高潮嗷嗷叫在线视频| 久久人人爽av亚洲精品天堂| 亚洲人成电影免费在线| 精品免费久久久久久久清纯 | 女人被躁到高潮嗷嗷叫费观| 丝袜美足系列| 国产一区二区 视频在线| 大片电影免费在线观看免费| 亚洲av欧美aⅴ国产| 国产精品久久久人人做人人爽| 亚洲全国av大片| 精品国内亚洲2022精品成人 | 一级黄色大片毛片| 中文字幕色久视频| 免费少妇av软件| 欧美精品亚洲一区二区| 国产亚洲精品一区二区www | 岛国在线观看网站| 91大片在线观看| 操美女的视频在线观看| 国产成人影院久久av| 一级片免费观看大全| 亚洲av电影在线进入| 亚洲精品美女久久av网站| 日韩视频在线欧美| 亚洲精品一区蜜桃| 黑人巨大精品欧美一区二区蜜桃| 99热全是精品| 欧美乱码精品一区二区三区| 99热网站在线观看| av超薄肉色丝袜交足视频| 天堂中文最新版在线下载| 国产精品久久久人人做人人爽| 蜜桃国产av成人99| 亚洲欧美精品综合一区二区三区| 亚洲精品av麻豆狂野| 久久久久久久久免费视频了| 久久久久久亚洲精品国产蜜桃av| 亚洲精品久久久久久婷婷小说| 大陆偷拍与自拍| 欧美日韩中文字幕国产精品一区二区三区 | 免费不卡黄色视频| 一边摸一边做爽爽视频免费| 精品免费久久久久久久清纯 | 大型av网站在线播放| 久久久久国内视频| 欧美日韩福利视频一区二区| 99热国产这里只有精品6| 一本—道久久a久久精品蜜桃钙片| 人妻久久中文字幕网| 国产高清国产精品国产三级| 热re99久久国产66热| 老熟妇乱子伦视频在线观看 | 丝袜喷水一区| 巨乳人妻的诱惑在线观看| 欧美精品高潮呻吟av久久| www.999成人在线观看| 国产成人精品久久二区二区91| 亚洲天堂av无毛| 老司机午夜福利在线观看视频 | 精品国产一区二区三区久久久樱花| 18在线观看网站| 99热国产这里只有精品6| 成人国产av品久久久| 性色av乱码一区二区三区2| 黄片大片在线免费观看| 69精品国产乱码久久久| 日本一区二区免费在线视频| 自拍欧美九色日韩亚洲蝌蚪91| 久久ye,这里只有精品| 中文字幕最新亚洲高清| 国产成人啪精品午夜网站| 国产免费视频播放在线视频| 亚洲中文日韩欧美视频| 不卡av一区二区三区| 亚洲精品第二区| 老司机靠b影院| 午夜影院在线不卡| 精品人妻熟女毛片av久久网站| 久久国产精品大桥未久av| 男女下面插进去视频免费观看| 国产av又大| 91大片在线观看| 日日夜夜操网爽| av电影中文网址| 美女视频免费永久观看网站| 一个人免费看片子| 亚洲男人天堂网一区| 免费观看av网站的网址| 一级,二级,三级黄色视频| 精品久久久久久电影网| 亚洲欧洲精品一区二区精品久久久| 一级毛片精品| 国产精品一区二区精品视频观看| 成人av一区二区三区在线看 | 黄片大片在线免费观看| 最新在线观看一区二区三区| 久久ye,这里只有精品| 国产在视频线精品| 亚洲欧美激情在线| 精品亚洲乱码少妇综合久久| 丝袜喷水一区| 大香蕉久久网| cao死你这个sao货| 久久久精品国产亚洲av高清涩受| 国产片内射在线| 在线十欧美十亚洲十日本专区| 欧美性长视频在线观看| 国产日韩欧美视频二区| 天天躁狠狠躁夜夜躁狠狠躁| 热99久久久久精品小说推荐| 香蕉丝袜av| 后天国语完整版免费观看| 国产亚洲午夜精品一区二区久久| 啦啦啦中文免费视频观看日本| 成年人午夜在线观看视频| 国产精品影院久久| 精品少妇黑人巨大在线播放| 亚洲国产精品一区二区三区在线| 后天国语完整版免费观看| 国产黄色免费在线视频| 亚洲人成电影免费在线| 日本wwww免费看| 亚洲成国产人片在线观看| 啦啦啦在线免费观看视频4| 亚洲午夜精品一区,二区,三区| 女人高潮潮喷娇喘18禁视频| 91麻豆精品激情在线观看国产 | 亚洲男人天堂网一区| 国产免费福利视频在线观看| bbb黄色大片| 丰满迷人的少妇在线观看| 不卡av一区二区三区| 999久久久精品免费观看国产| 日韩制服丝袜自拍偷拍| 热99久久久久精品小说推荐| 欧美激情高清一区二区三区| 波多野结衣一区麻豆| 国产麻豆69| 青青草视频在线视频观看| 欧美日韩精品网址| 国产真人三级小视频在线观看| 亚洲av电影在线进入| 视频在线观看一区二区三区| 久久久国产一区二区| 91老司机精品| 久久久精品区二区三区| 国产欧美日韩一区二区三 | 欧美精品一区二区免费开放| 亚洲国产精品一区三区| 久久久久国产精品人妻一区二区| 亚洲国产看品久久| 久久人妻福利社区极品人妻图片| 久久精品久久久久久噜噜老黄| 国产成人免费无遮挡视频| 韩国高清视频一区二区三区| 国产不卡av网站在线观看| 亚洲一区二区三区欧美精品| 男女高潮啪啪啪动态图| 日韩 亚洲 欧美在线| 久久久精品免费免费高清| 人成视频在线观看免费观看| 亚洲第一欧美日韩一区二区三区 | 国产精品偷伦视频观看了| 精品一区在线观看国产| 一本久久精品| 国产成人系列免费观看| 免费高清在线观看日韩| 亚洲人成电影免费在线| 久久 成人 亚洲| 纯流量卡能插随身wifi吗| 99精品欧美一区二区三区四区| 久久精品成人免费网站| 国产成人啪精品午夜网站| a 毛片基地| 精品一品国产午夜福利视频| 久久99一区二区三区| e午夜精品久久久久久久| 久久精品国产综合久久久| 精品亚洲乱码少妇综合久久| 久久久国产精品麻豆| 在线观看免费午夜福利视频| 亚洲情色 制服丝袜| 亚洲国产精品成人久久小说| 青春草视频在线免费观看| 久久精品国产亚洲av高清一级| 夜夜夜夜夜久久久久| 超碰成人久久| tube8黄色片| 最近最新中文字幕大全免费视频| 两人在一起打扑克的视频| 人人澡人人妻人| 一边摸一边做爽爽视频免费| 日韩欧美一区二区三区在线观看 | 精品福利永久在线观看| 大码成人一级视频| 国产成人免费无遮挡视频| 国产精品国产三级国产专区5o| 蜜桃在线观看..| 亚洲av国产av综合av卡| 老司机福利观看| 丝袜脚勾引网站| h视频一区二区三区| 青草久久国产| 啦啦啦视频在线资源免费观看| 黄色视频在线播放观看不卡| 久久毛片免费看一区二区三区| 亚洲av国产av综合av卡| 久久久久久久久免费视频了| 超碰97精品在线观看| 黑丝袜美女国产一区| 久久久久视频综合| 欧美日韩av久久| 久久久精品免费免费高清| 久久久久久久久久久久大奶| av天堂久久9| 免费在线观看影片大全网站| 90打野战视频偷拍视频| 亚洲成国产人片在线观看| 中文字幕精品免费在线观看视频| 免费黄频网站在线观看国产| 国产成人精品久久二区二区91| 欧美少妇被猛烈插入视频| 老汉色∧v一级毛片| 国产一区二区激情短视频 | 婷婷色av中文字幕| 国产一区二区激情短视频 | 久久精品国产a三级三级三级| 国产成人精品在线电影| 一区二区av电影网| 亚洲欧美清纯卡通| 男女午夜视频在线观看| 狠狠狠狠99中文字幕| 高清av免费在线| 一边摸一边做爽爽视频免费| www.999成人在线观看| 国产成人一区二区三区免费视频网站| 天天躁日日躁夜夜躁夜夜| 男女无遮挡免费网站观看| 中亚洲国语对白在线视频| 国产人伦9x9x在线观看| 亚洲精品国产av蜜桃| 大陆偷拍与自拍| 国产男女内射视频| 黑人巨大精品欧美一区二区mp4| 老汉色av国产亚洲站长工具| 视频区图区小说| 美女国产高潮福利片在线看| 高清视频免费观看一区二区| 欧美人与性动交α欧美精品济南到| 久久国产亚洲av麻豆专区| 国产又爽黄色视频| 91国产中文字幕| 国产成人a∨麻豆精品| 日本91视频免费播放| 一级,二级,三级黄色视频| 日日摸夜夜添夜夜添小说| 欧美精品一区二区大全| 法律面前人人平等表现在哪些方面 | 在线十欧美十亚洲十日本专区| 国产av一区二区精品久久| 美女主播在线视频| 日韩免费高清中文字幕av| 午夜免费观看性视频| 欧美精品一区二区免费开放| 欧美日韩国产mv在线观看视频| av欧美777| av福利片在线| 老司机亚洲免费影院| a级片在线免费高清观看视频| av片东京热男人的天堂| a 毛片基地| 捣出白浆h1v1| 精品久久蜜臀av无| 热re99久久精品国产66热6| 国产精品一区二区在线观看99| 国产精品欧美亚洲77777| 欧美亚洲日本最大视频资源| 大陆偷拍与自拍| av一本久久久久| 国产在线一区二区三区精| 国产成人精品久久二区二区91| 欧美激情高清一区二区三区| 欧美精品一区二区免费开放| 高清欧美精品videossex| 午夜免费观看性视频| 久久久精品国产亚洲av高清涩受| 国产精品1区2区在线观看. | 日本vs欧美在线观看视频| 亚洲欧美激情在线| 叶爱在线成人免费视频播放| 9色porny在线观看| 欧美av亚洲av综合av国产av| 亚洲精品久久久久久婷婷小说| 亚洲av片天天在线观看| 国产av一区二区精品久久| 免费不卡黄色视频| 999久久久精品免费观看国产| 国产伦人伦偷精品视频| 淫妇啪啪啪对白视频 | 满18在线观看网站| 黄色毛片三级朝国网站| 80岁老熟妇乱子伦牲交| 十分钟在线观看高清视频www| 亚洲五月色婷婷综合| 国产成人精品久久二区二区91| 色播在线永久视频| a级片在线免费高清观看视频| 99久久精品国产亚洲精品| 亚洲精品在线美女| 永久免费av网站大全| 美女福利国产在线| 黄片小视频在线播放| 可以免费在线观看a视频的电影网站| 欧美日韩黄片免| 人成视频在线观看免费观看| 美女福利国产在线| www.999成人在线观看| 首页视频小说图片口味搜索| 男人爽女人下面视频在线观看| 色94色欧美一区二区| 欧美大码av| 男人添女人高潮全过程视频| 日韩有码中文字幕| 一级黄色大片毛片| 免费女性裸体啪啪无遮挡网站| 淫妇啪啪啪对白视频 | 免费高清在线观看日韩| 亚洲欧洲日产国产| 99久久人妻综合| 两性夫妻黄色片| 色婷婷久久久亚洲欧美| 中文字幕人妻丝袜一区二区| 精品熟女少妇八av免费久了| 精品少妇一区二区三区视频日本电影| 精品久久久久久久毛片微露脸 | a 毛片基地| 久久人妻福利社区极品人妻图片| 一级毛片女人18水好多| 日韩 欧美 亚洲 中文字幕| 亚洲欧美成人综合另类久久久| 9热在线视频观看99| 亚洲人成77777在线视频| www.精华液| 国产野战对白在线观看| 亚洲美女黄色视频免费看| 手机成人av网站| 久久人妻福利社区极品人妻图片| 看免费av毛片| 久久中文看片网| 夫妻午夜视频| 亚洲欧美色中文字幕在线| 久9热在线精品视频| 超碰成人久久| 十八禁网站网址无遮挡| 午夜成年电影在线免费观看| 国产野战对白在线观看| 成人黄色视频免费在线看| 下体分泌物呈黄色| 久久人妻福利社区极品人妻图片| 色视频在线一区二区三区| 欧美午夜高清在线| 高清av免费在线| 一个人免费看片子| bbb黄色大片| 欧美日韩黄片免| 久久久久久久久久久久大奶| 午夜福利影视在线免费观看| 日本黄色日本黄色录像| 亚洲欧洲精品一区二区精品久久久| 亚洲成人免费av在线播放| 最黄视频免费看| 一级黄色大片毛片| 满18在线观看网站| 免费在线观看视频国产中文字幕亚洲 | 91成年电影在线观看| 中国国产av一级| 国产淫语在线视频| 在线av久久热| 无遮挡黄片免费观看| 国产熟女午夜一区二区三区| 黄色视频在线播放观看不卡| 肉色欧美久久久久久久蜜桃| 亚洲国产欧美网| 美女高潮到喷水免费观看| 日本av手机在线免费观看| 日韩欧美一区二区三区在线观看 | 欧美性长视频在线观看| 日韩三级视频一区二区三区| 久久午夜综合久久蜜桃| 精品一区二区三区av网在线观看 | 国精品久久久久久国模美| 国产精品二区激情视频| 国产亚洲午夜精品一区二区久久| 在线观看一区二区三区激情| 色婷婷av一区二区三区视频| 久久精品国产a三级三级三级| 人人妻人人澡人人看| 老熟妇仑乱视频hdxx| 免费看十八禁软件| 岛国在线观看网站| 亚洲九九香蕉| 国产精品久久久av美女十八| 亚洲精品国产av蜜桃| 国产免费av片在线观看野外av| 一进一出抽搐动态| 动漫黄色视频在线观看| 亚洲熟女精品中文字幕| av在线app专区| 久久久久国产一级毛片高清牌| 国产主播在线观看一区二区| 国产精品欧美亚洲77777| 99精品欧美一区二区三区四区| 少妇猛男粗大的猛烈进出视频| 国产精品自产拍在线观看55亚洲 | 亚洲欧美一区二区三区久久| 啪啪无遮挡十八禁网站| 天堂俺去俺来也www色官网| 国产一区二区三区av在线| 乱人伦中国视频| e午夜精品久久久久久久| av视频免费观看在线观看| 一级毛片精品| 99国产精品一区二区蜜桃av | 高清欧美精品videossex| 中国美女看黄片| 好男人电影高清在线观看| 人妻久久中文字幕网| 在线精品无人区一区二区三| 亚洲va日本ⅴa欧美va伊人久久 | a级毛片黄视频| 一区二区三区精品91| av线在线观看网站| 免费av中文字幕在线| 日本黄色日本黄色录像| 日日夜夜操网爽| 满18在线观看网站| 午夜视频精品福利| 一级片'在线观看视频| 精品少妇黑人巨大在线播放| 亚洲av成人一区二区三| 90打野战视频偷拍视频| 侵犯人妻中文字幕一二三四区| 精品熟女少妇八av免费久了| 欧美精品高潮呻吟av久久| 国产日韩一区二区三区精品不卡| 日韩视频一区二区在线观看| 亚洲精品一卡2卡三卡4卡5卡 | 五月天丁香电影| 午夜精品久久久久久毛片777| 亚洲成人免费av在线播放| 久久影院123| 国产精品av久久久久免费| 麻豆乱淫一区二区| e午夜精品久久久久久久| 日韩欧美一区视频在线观看| 亚洲 欧美一区二区三区| 久久99一区二区三区| 黄色 视频免费看| 亚洲国产欧美在线一区| 精品人妻熟女毛片av久久网站| av电影中文网址| 中国美女看黄片| 日本五十路高清| 久久久精品94久久精品| 国产在线视频一区二区| 亚洲国产精品成人久久小说| 成人黄色视频免费在线看| 无遮挡黄片免费观看| 制服人妻中文乱码| 久久中文字幕一级| 久久久久久免费高清国产稀缺| 18禁裸乳无遮挡动漫免费视频| 一本一本久久a久久精品综合妖精| 丰满少妇做爰视频| 国产黄频视频在线观看| 免费少妇av软件| av国产精品久久久久影院| 国产亚洲精品久久久久5区| 国产免费视频播放在线视频| 1024香蕉在线观看|