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6b _D1b-WP2_ hydrological_BfG

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FloodMan

Updated hydrological models with EO-Data

Deliverable no 6b (D1b-WP2)

Peter Krahe, Claudia Rachimow, Matthias Hammer (all BfG)

Contract: EVG1 – CT – 2002- 00085

Near real-time flood forecasting,

warning and man agement system based on satellite radar images, hydrological and

hydraulic models and in-situ data

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Updated hydrological models with EO-Data (BfG)

Contents

1Abstract 52Introduction 53

Methodologies 63.1The River Sieg basin 63.2Hydrological Models 93.3Model calibration 113.4Data assimilation

144

Demonstration of data assimilation methodologies

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Updated hydraulic models with EO-Data (BfG)

DOCUMENT AUTHORISATION

Function Name

Date Signature

Author

Peter Krahe, Claudia

Rachimow, Matthias Hammer

1-4-04

Checked by Authorised by

DOCUMENT STATUS SHEET

Version Date Section Change(s)

0.5

1-4-05

All

Draft document released for the project consortium only

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Updated hydrological models with EO-Data (BfG)

ACRONYMS

APPLICABLE AND REFERENCE DOCUMENTS

Francois, C. , Quesney, A. and Ottlé, C. (2003): Sequential Assimilation of ERS-1 SAR

Data into a Coupled Land Surface–Hydrological Model Using an Extended Kalman Filter. Journal of Hydrometeorology, V. 4, 473-487Houser, P. R., W. J. Shuttleworth, J. S. Famiglietti, H. V. Gupta, K. Syed, and D. C.Goodrich, 1998: Integration of soil moisture remote sensing and hydrologic modeling using data assimilation. Water Resour. Res., 34, 3405–3420.El Serafy, G.Y. (2003): Comparison of EKF and EnKF in Sobek River. Report, WL Delft Hydraulics, Delft

Valentijn, P., Hueben, R., Verhoest, N, Francois, P., De Troch, F. and Troch, P. (2002):

Improvement of TOPLATS-based discharge predictions through assimilation of ERS-based remotely sensed soil moisture values. Hydrol. Process. 16, 995-1013William L., Laymon, C., Inguva, R. and M. Schamschula (2002): Assimilating remote sensing data in a surface flux-soil moisture model. Hydrol. Process. 16, 1645-1662

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Updated hydraulic models with EO-Data (BfG)

Abstract

The progress in hydrological modelling for the River Sieg basin, and in the development of data

assimilation methodologies for using remotely sensed soil moisture estimates in rainfall-runoff models are reported. For the River Sieg basin the rainfall-runoff model HBV-BfG was set up with special regard to it’s use in data assimilation schemes. Furthermore, two flow routing models were established for the course of the River Sieg.

Different data assimilation techniques were examined and evaluated with special emphasis of their application in operational flood forecasting. Based on this study three approaches, the Statistical Correction Method (SCM), the Extended Kalman Filter (EK) and the Ensemble Kalman Filter (EnK) are chosen for testing their capabilities to include surface soil moisture derived from satellite data in the production scheme of a semi-distributed rainfall-runoff model.

2 Introduction

The main objective is to assess satellite based soil moisture tools in operational flood forecasting system based on observed and forecasted meteorological variables in combination with a River Basin Model (RBM). One of the RBM’s which is in operational use in Germany as well in The Netherlands consists of the rainfall-runoff model HBV-96 and the1-d hydrodynamic models WAVOS and SOBEK. In this part of the study improvement of the rainfall-runoff model will be examined. The problem of imperfect initial states and the uncertainty of the meteorological input data form a serious problem in the application of rainfall-runoff models in flood forecasting praxis. Therefore, methodologies are needed to overcome these obstructions.

A first attempt to sequentially assimilate European Space Agency (ESA) Remote Sensing Satellite (ERS) synthetic aperture radar (SAR) estimations of surface soil moisture in the production scheme of a lumped rainfall–runoff model will be conducted. Three methods the Statistical Correction Method (SCM), the Extended Kalman Filter (EK) and the Ensemble

Kalman Filter (EnK), which are well known from the literature to be able to assimilate the SAR retrievals in a land surface scheme will be tested in detail. The various assimilation procedures will be tested, corresponding to SAR measurements which will be carried out in a special field campaign in the time period November 2004 up to March 2005.

This work will be carried out in four phases:

1) Setting- up of procedures for preparation of meteorological input data and hydrological models,

2) Development of data and assimilation methodology sub-divided in the tasks analyses of available methodologies, evaluation and selection of specific methodologies, and finally in software development,

3) Demonstration of the feasibility of the methodologies by carrying out quasi-operational flood forecasts for the River Sieg and the stretch of the River Rhine between the gauges Andernach and Düsseldorf,

4) Conclusions and recommendations for data handling of satellite data and their use in hydrological models used for operational flood forecasts.

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Updated hydrological models with EO-Data (BfG)

The improvements observed in simulating flood events in a quasi-operational mode will

demonstrate the potential of sequential assimilation techniques for monitoring surface functioning models with remote sensing data.3

Methodologies

3.1

The River Sieg basin

This study will be performed in the River Sieg basin (2.825 km2), which represent a major tributary of the river Rhine along the river stretch between gauge Andernach and gauge Düsseldorf. The basin is located on the transition zone between the so called Middle Rhine and the Lower Rhine. A large portion of the River Sieg basin consists of upland areas, while the lower part of the River Sieg is located in the so called

…Niederrheinische Bucht“, which is a typical lowland area.

Fig. 1 River Sieg basin with sub-basins for rainfall-runoff modelling and main gauging stations

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Updated hydraulic models with EO-Data (BfG)

Table. 1 Catchment area and reference gauges for sub-basins of the river Sieg

Sub-basin

Abbreviation Gauging station Catchment area [km 2]Main Tributaries

Upper Sieg OBSG Betzdorf 754Ferndorf , Heller Middle Sieg MISG Eitorf 714Nister , Wipperbach Agger AGSG Lohmar 805Sülz Lower Sieg UNSG

Menden

552Br?l

Sieg total

2825

The land use of the river Sieg basin is depicted in Fig.2. The predominant land use class is forest (~ 64%) followed by meadow (27%) and 7% is occupied by urban areas. Approximately 2% is agricultural area, only.

Fig. 2Land use in the river Sieg basin

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Updated hydrological models with EO-Data (BfG)

The water balance of the River Sieg basin can be characterised by the annual mean values of the

water balance components (s. Table 2) and by the main statistical data of discharge (s. Table 3).The mean annual precipitation of the river Sieg basin adds up to 1200 mm, while the real evapotranspiration amounts 540 mm. Therefore, 660 mm/a, (59 m3/s) of annual runoff was observed in the time period 1961-1990.

Table. 2 Water balance components for the river Sieg basin for the time period 1961 - 1990

Sub-basin

A Area

P Precipitation (corr.)

Er Evaporation R = P - Er Runoff Reference gauge Q

Discharge

[km2][mm/a]

[mm/a][mm/a][m3/s][m3/s]Obere Sieg

754124753371417.1Betzdorf 17.1Mittlere Sieg 714

115254061213.9Eitorf 30.9Agger

805130055374719.1Lohmar 19.1Untere Sieg

55210605445169.09.0EG Sieg 2825120254365959.0

Menden

59.0

Table. 3 Main statistical data in [m3/s] after [DGJ 1995]

Gauging station MQ MNQ NQ MHQ HQ Time series Betzdorf 15.6 1.640.63199516

(7.2.1984)1973-1995Eitorf 27.4 3.13 1.28339692

(7.2.1984)1971-1995Lohmar 17.2 2.250.84186385

(23.2.1970)1951-1995Menden

53.5

6.43

2.40

574

1050

(7.2.1984)

1965-1995

Floods affect the River Sieg basin often. This happens mainly during the hydrological winter half year, especially from December up to March. These floods are producing high damages within the catchment itself, but also downstream in the river Rhine. For example, the River Sieg played an important role during the extreme flood of January 1995. On 30.1.1995 the discharge at gauge Cologne was 10.940 m3/s, which corresponds to a flood with a return period of 45-70 years. The discharge at gauge Menden contributes with 653 m3/s to this peak. The high potential of damages due to a flood can be seen in Fig. 3, where the location of the urbanised areas are illustrated.

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Updated hydraulic models with EO-Data (BfG)

Fig. 3

River Sieg basin with sub-basins for rainfall-runoff modelling, main gauging stations, and location of urbanised areas

3.2 Hydrological Models

For modelling the response of the river Sieg basin to meteorological forcing, especially

precipitation, a model system was set up which consist of a rainfall-runoff model simulating the runoff generation and concentration within a sub-basin and an independent working water

transport model, which links the runoff of the sub-basin together, and simulates the flood routing processes in the river and over the floodplain.

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Updated hydrological models with EO-Data (BfG)

The model used in this study for rainfall-runoff modelling is the hourly conceptual semi-distributed model HBV-BfG., This model is semi-distributed, which means that the sub-basin

which has to be modelled is subdivided in height zones (typically height zones with a 100 m range are chosen). Each height zone can be subdivided in different land use classes. Land uses classes and their parameterisation can be defined within the model. So far, only the two classes forest areas and non forest areas are selected in order to be comparable to the system, which is in use for operational flood forecasting.

The input to the rainfall-runoff model is the hourly areal mean precipitation and areal mean air temperature. The lumped meteorological input for a sub-basin is distributed to the height zones under consideration of the height. The potential evapotranspiration is handled in the available version by the use of long term monthly daily means of the so called Grass-Reference

evapotranspiration. This can be handled as long as floods of the hydrological winter half will be simulated and forecasted.

Two different hydrological Water Transport Models called WTM-LagDamp and WTM-ConDiff were developed for simulating the flood routing. Each of them representing different solutions of the so called Convection-Diffusion equation which itself is a simplification of the well known de Saint-Venant equations. This model approaches are widely used in operational flood forecasting models for describing 1-d water flows in rivers. The use of the simplified equations which is

although named as the kinematic approach are allowed in head waters and in modelling the water flows in distributed river networks. A spatial structure represented by knots was set up for the river Sieg basin (Table 4). The spatial sub-division takes into account the mathematical model assumptions as well as the location of the main tributaries along the River Sieg.

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Updated hydraulic models with EO-Data (BfG)

Table. 4Spatial structure of the WTM’s LagDamp and ConDiff for the River Sieg

River basin

Knot Factor Sub-basins of HBV-BfG

River basin Catchment area [km2]

K 0...1Name Catchment area [km2]

Reference gauge

SB1Obere Sieg 754K1 1.0OBSG 754Betzdorf

SB2

Nister

217K2 1.0SB3Wipperbach 246K2 1.0K30.5SB4251K4

0.5MISG 714Eitorf

SB574

K5 1.0SB6Br?l 217K5 1.0SB7Hanfbach 126K6 1.0SB8Pleisbach 135K7 1.0UNSG 552Menden

SB9

Agger

805

1.0

AGSG 805Lohmar

3.3 Model calibration

The hydrological models were calibrated manually (trial and error) under assignment of the

quality criteria mentioned in the part of hydraulic modelling, and based on data of the time period 1990/1994. An overview of the quality is given in Table 5 and in hydrographs for selected gauging stations depicted in Fig. 4. The model was verified for the time period 1995/1999.

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Updated hydrological models with EO-Data (BfG)

Fig. 4

Hourly simulation with rainfall-runoff model HBV-BfG for the Upper Sieg basin at gauge Betzdorf/Sieg for the flood of November/December 1991

Table 5Model quality of HBV-BfG in the calibration and verification periods

Gauge

Nash-Sutcliffe

RMSPE Betzdorf 0.8770.743Calibration period (1990-1994)Lohmar 0.7990.605Betzdorf 0.8530.538Verification period (1995-1998)Lohmar 0.767 5.3041Betzdorf 0.8620.660Total

(1990-1998)

Lohmar

0.786

3.5651

low value is a result of measurement errors on 15. and 18. 9. 1998

In the same way the model parameters of the WTM models were derived (s. Fig. 5). Additionally,hydraulic parameters such as mean discharge, water level, flow velocity, hydraulic radius , area,and volume were calculated based on cross sections, DEM and a 1-d stationary water level calculation (Fig. 6). Based on this data the model parameters of the WTM models can be calculated.

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Updated hydraulic models with EO-Data (BfG)

Fig. 5

Validation of rainfall-runoff model HBV-BfG and the WTM-ConDiff model for the Upper Sieg basin at gauge Betzdorf/Sieg and at the outlet of the River Sieg at Gauge Menden for the flood of November 1998

Fig. 6

Location of cross sections and discharge values with a return period of 5, 10, 25, 50 and 100 years , and the derived hydraulic parameters

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Updated hydrological models with EO-Data (BfG)

3.4

Data assimilation

With regard to the data assimilation and uncertainty, hydrological modelling procedure is

splitted up in three autonomous parts:

1) Preparation of hydrometeorological input data (PREMET)

2) Modelling the runoff generation and runoff concentration within sub-basins by use of HBV-BfG

This model type is used on the one hand due to its application in the operational flood forecasting for the river Rhine, but also due to the fact, that this model type is appropriate to test different assimilation procedures. The reasons for this are

constitute in its structure, e.g. the disconnection between soil and runoff storages, and in the robustness of the underlying equations and parameters. Also, the model can be used in a distributed and in a semi-distributed mode. The disconnection of soil and runoff storages allows the combination of the model or parts of the model with more sophisticated models for modelling the Soil-Vegetation-Atmosphere processes, e.g.by the so-called SVAT models. These facts allow the extension of the hydrological model, which is in use for operational flood forecasting step by step, if necessary.A special focus lies on the write out function of the different water storages such as snow water equivalent and soil moisture as well as runoff storages.

3) Modelling the flow routing by independent working WTM’s. They encompasses the linkage of the runoff of different sub-basins to the outlet of the river basin under study. A special focus lies on the derivation of the model parameter values out of hydraulic variables. Especially, the flooded area and the related water volume stored in a river reach including the flood plain were taken into account. This makes this kind of models feasible to use spatially distributed information, e.g. satellite derived flood area and derived border lines, for data assimilation.

To get an impression, what is the influence of the initial states of a hydrological model sensitivity a study was carried out by changing the initial soil state. One result is depicted in Fig. 7.

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Updated hydraulic models with EO-Data (BfG)

Fig. 7

Response of the Upper Sieg basin at gauge Betzdorf/Sieg to different initial states of soil moisture at the beginning of the simulation period

Based on a literature study different data assimilation methods were analysed with regard to the issue of using remote sensed soil moisture data in hydrological models.The objective of this exploration was:

? how useful are remotely sensed data in estimating soil moisture,

? how can they be applied in hydrological models in a way that minimises their inherently

deficient spatial (in the vertical direction) and temporal resolutions,

? and how can they be incorporated and improve operational flood forecasts?

It was found out that the following methods were useful for further elaboration and testing within the River Sieg basin:

? Statistical Correction Method (SCM)

Valentijn et al. (2002) investigate the possibility to improve discharge predictions from a lumped hydrological model through assimilation of remotely sensed soil moisture values. Besides the development of an algorithm to estimate surface soil moisture values through active microvave remote sensing, the remotely sensed soil moisture values over bare soils are then assimilated into a hydrological model using the statistical correction method. The results suggest that it is possible to determine soil moisture values over bare soils from remote sensing observations without the

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Updated hydrological models with EO-Data (BfG)

need to collect ground truth data, and that there is potential to improve model based discharge

predictions through assimilation of these remotely sensed soil moisture values.

The hydrological model used in their study was the TOPLATS model, which can be run in a fully distributed and in a statistical mode. The statistical mode was used in their study. The statistical correction method was originally developed by Houser et al. (1998). In this method, the statistics of the remotely sensed soil moisture values are assumed to be correct. The soil moisture content of the upper soil layer is adapted by rescaling the modelled soil moisture by the standard

deviations of the remotely sensed observed and the modelled soil moisture. In the further steps the mean of both variables are taken into account.

When the soil moisture content of the upper layer is adapted, the soil moisture content of the lower layer is modified, as a weighted average between an update to the same relative amount as the upper layer at the top of the lower layer.

This method fulfils the requirements of a operational flood forecasting system especially in the point of robustness and simplicity, even some problems has to be solved for application in real flood forecasting applications. Therefore, this methodology will be examined and applied within the Floodman project.

? Extended Kalman Filter (EKF)

A Kalman Filter provides an optimal solution based on both measurements and model estimates (William et al., 2002). This approach has the advantage of coupling the space-time continuity of a surface-flux models with intermittent remote observations in a framework that balances model and measurement uncertainties. The intermittent observations are used to nudge the model state toward the observation by the classic extended Kalman filter problem of a stochastic-dynamic non-linear system.

A first attempt to sequentially assimilate European Space Agency (ESA) Remote Sensing Satellite (ERS) synthetic aperture radar (SAR) estimations of surface soil moisture in the

production scheme of a lumped rainfall–runoff model was conducted by Francois et al, 2003. The methodology, which was developed, is an extended Kalman filter to assimilate the SAR retrievals in a land surface scheme represented by a simple two-layer hydrological model. The

improvements observed in simulating flood events demonstrate the potential of sequential assimilation techniques for monitoring surface functioning models with remote sensing data.? Ensemble Kalman Filter (ENKF)

The Potential of Ensemble Kalman Filtering was proven for the hydrodynamic modelling Sobek model by El Serafy (2003). She came to the conclusion that application of this data assimilation techniques in flood forecasting is feasible, although the computational burden might still be an obstacle. The techniques itself are relatively simple to implement in a generic way. Both

approaches EKF and ENKF providing comparable results. The advantage of the ENKF is that it has not to be implemented in a model equations.

The solutions of the data assimilation problem found in the literature with regard to the use of remotely sensed soil moisture data are encouraging. However, there are many issues that must be

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Updated hydraulic models with EO-Data (BfG)

overcome in order to implement such kind of assimilation systems successfully. The most

important issues are:

? Inaccurate meteorological input data,

? Long periods of missing remotely sensed data,? Effects of scale and surface heterogeneity,? Vegetation effects,? surface roughness,

This work will be carried out in four phases:

1) Setting- up of procedures for meteorological input data and different hydrological models,2) Development of data and assimilation methodology sub-divided in the tasks analyses of

available methodologies, evaluation and selection of specific methodologies and finally in the software development,

3) Demonstration of the feasibility of the methodologies by carrying out quasi-operational flood

forecasts for the River Sieg and stretch of the River Rhine between Andernach and Düsseldorf,

4) Conclusions and recommendations for data handling of satellite data and their use in

hydrological models used for operational flood forecasts.

4 Demonstration of data assimilation methodologies

Based on the results obtained so far, it has to be concluded that a clear model framework has to be developed and it’s suitability has to be proven by application of this framework on synthetic as well as on real life data. With this in mind the demonstration phase was started in November 2004which will continue up to March 2005.

The following tasks will be carried out based on the data of the so called “field campaign” :

? Different data sets of meteorological input data will be collected, and the error variances required by the assimilation procedures will be calculated,

? The soil moisture data derived from the remote sensing data will be prepared for their use in the data assimilation procedures,

? Quasi-operational flood forecasts will be carried out with and without application of the data assimilation methodology By comparing the results the feasibility and the benefits of the developed procedures will be shown. Furthermore, conclusions and recommendations for data handling of satellite data and their use in hydrological models used for operational flood forecasts will be given. In Figure 8 the hydrograph of water level at gauge Menden/Sieg and gauge K?ln/Rhine are depicted. Within the demonstration phase three floods occurred in the River Sieg basin which allows the demonstration of the procedures.

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Updated hydrological models with EO-Data (BfG)

010020030040050060070001.09

21.09

11.1031.1020.1110.1230.1219.0108.0228.02

2004/2005

[c m ]

Fig. 8Water level at gauge Menden/Sieg and gauge K?ln/Rhine in the field campaign 2004/2005

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神之墓地2.6a攻略通关主要是看你能守住家不 BOSS不难难的是小怪前期比较难守的是6波和9波以后的魔免怪守的时候不能有地狱火去抗要买骷髅杖招骷髅去抗自己在后面打守住这些了后面就好守了前2个BOSS 杀的时候最好用地狱火砸他因为砸的时候是带晕的 BOSS基本都是晕到死的不咋又人皇的沉默也好只要前面2个ＢＯＳＳ打了后面就简单了右下角灵兽爆灵丹河道螃蟹爆治疗之手左边河道上边妖皇爆浩劫妖皇令妖皇骨灰妖皇下面食尸鬼巫师爆致命毒素可以合毒素球最左边的中间小怪爆厄运封魔石领主爆曙光镇灵石地狱火爆命运魂之碎片小阿爆永恒诅咒魄之碎片往右边点火凤凰爆幽冥鬼火上面英雄区昊天爆空间之刃作者爆绝世凶器冰魂右边河道上去点绝天爆天书再右边蓝龙爆龙盾红龙爆龙晶黑龙爆龙之号角黄龙爆龙符绿龙爆生生不息再往上去点左边守护者爆星辰书加基地5000防的冰爷爷爆魔杖传送贯穿不用说了吧裂天=传送真+贯穿真+神力结晶苍穹=传送真+空间之刃+昊天的心脏（任务）魔化浩劫=浩劫+妖皇骨灰丧魂龙刀=龙之号角+龙族至宝幽冥鬼爪=剑魂+幽冥鬼火+粉碎剑魂妖龙号角=龙之号角+妖皇骨灰（上山打老虎合）其他的装备都买的到了任务1 传说魄之力量去找昊天觉醒（让他杀）有几率的觉醒了去训练1房间的下面找那个女人有几率触发任务的再去杀昊天一定要把空间刃爆出来然后在12-13点去找昊天然后回到那女人那昊天叫你找他的心脏然后带神力结晶（守墓老人获得）满地图找心脏了找到了永囚禁锢他然后去找昊天苍穹就有了任务2 带贯穿真杀了绝天拿绝天爆的天书找冰爷爷他给你信物然后杀守护者爆星辰书去找守墓老人成了真半神把星辰书给守墓老人了找血饮他给你个布娃娃带个浩劫骨灰布娃娃去找隐龙魔化浩劫了就在隐龙旁边找忘尘任务就完了

神之墓地2.6d攻略

神之墓地2.6D龙神单通详细攻略龙神是神之墓地中很热的一个英雄，不仅仅是因为帅，很有型头，而且隐藏任务挺多，技能绚丽，龙神单通还是有点难度的，我也是费了一段时间才能顺利通关的，下面把我的心得体会跟大家说说，希望对新手有一定的知道作用。先show一下我最后龙神的属性跟装备：属性: 白属性（不算装备）力量16万+，敏捷15万+，智力没注意，8万左右。装备丧魂龙刃神之卷-残卷弑神裂天还是皓月来着，俩武器名记混了（传说真+空间合成的那个）剑魂（2.5B最后35波的时候要和出鬼爪）魔化的甲 1、一出生立刻去复活点把蓝补满。 2、小龙去开左边螃蟹的视野。 3、迅速去打食人魔的血液，路过胖妞的时候买3个毒液球，先打够6个换10字架（变身打，顺便打个治愈之手）。 4、在换10字架的时候怪也靠近老家了，这时候系统给你2木头，换钱，然后用小龙找胖妞，买杀100进攻怪的任务，买一个地狱火。 5、龙神得到十字架立刻Hg,去出生点满蓝，顺便用-h命令把仓库放到基地下方（离胖妞近点，方面买任务），然后去2号练功房。

6、变身好之前小龙身上要有一个护盾（地狱火+闪避+毒液），一个地狱火，这样小龙一次可以招两个地狱火。 7、再有钱了，就在仓库里也放一个护盾，一个地狱火，这样一次可以招4个地狱火。地狱火随着英雄升级也变的厉害，足够帮龙神守住前期的怪（地狱火魔免，狮鹫以及后面加纳海妖前后的怪都不攻击地狱火，英雄守--后面详解）。 8、变身好了，hg，顺便再买个球，这样英雄的装备是“十字架+治愈手+护盾+3个毒液球”，如果家里堆积的怪多了，就放个5级小招灭一下，然后迅速进钱房。 9、进去之后立刻变身，原地不动的话右边的怪应该过来打你，不打的话就动一下。 10、点护盾招地狱火，把左边的树打了，控制地狱火引左边的怪。左边的怪全部集中到中间的话，新的怪会刷新。护盾技能好了再把右边的树也打掉。 11、变身结束之前hg（小心别死了），复活点满蓝，家里堆积的怪多了就放个小招。 12、1号练功房打怪，等变身好就重复上面的操作。 13、3波左右，英雄50级了就可以长混钱房，很辛苦，变身没有就要左右跑，如果5级技能可以秒钱怪了，多多利用。 14、英雄很快100级(任务完成立刻接)，学了恶魔气息，直接去木头房。上下两边的木头怪都打一下，然后跑到中间，门跟回城点之间的地方站好。然后两边的木头怪会源源不断的来打你，木头呼呼的就涨起来了。 15、有了木头迅速出武器跟甲，武器出传说。再刷的过程中，如果来魔免怪了，英雄就hg一路向上跑，恶魔气息会杀掉靠近你的怪，等到跑到足够远了立刻回城进木头房，上面的木头放一个技能秒掉，下面的平砍（要3级甲才能去平砍，否则会挂）。 16、甲4级之后去打封魔石、镇魔石升级武器，至于魂之碎片，打的时候小心点，出了还好，小心别死了。。。魄之碎片就算了吧，你的打不了。。。 17、继续刷树攒木头，刷到2500就买个聚能魔刃，那样赚木头的速度就快了近一倍。两个木头房来回飞着刷，恶魔气息是多少可以秒树人我忘记录了。。。

神之墓地攻略(全)

任务4：守墓老人的恐怖试炼接受地点：无须接受【默认】任务过程：选择英雄处的下方有个守墓老人，掌握半神之力前接近他，有一定几率获得他的认可，得到物品【神力结晶】，失败则死亡，等级下降10级。任务5：小禽兽的猥琐心理（英雄人皇的专属任务）接受地点：无须接受【默认】任务过程：人皇200级后接近基地上方的小禽兽，100%获得装备【噬心戒】，同时小禽兽停止释放技能青蛙王子。任务6：虚无之守护接受地点：无须接受【默认】任务过程：任何英雄200级后不停的接近浮云宫大宫主有几率获得物品【虚无之守护】（虚无之守护是开启腐朽之地大门的钥匙）任务7：传说之剑的觉醒接受地点：无须接受【默认】任务过程：携带【传说之剑-魄之力量】时被昊天攻击，有几率觉醒为【传说之剑-真】任务8：贯穿天地的妖化接受地点：无任务过程：持有【贯穿天地-永恒诅咒】后，杀死任意敌人有几率妖化为【贯穿天地-真】（几率低下，需大规模刷怪）任务9：妖皇与魔帝的恩仇接受地点：无任务过程：携带【深渊魔甲MAX】和【妖皇的骨灰】进入魔帝墓地，魔帝的灵魂将给【深渊魔甲MAX】注入魔气，获得物品【深渊魔甲-魔化】（魔帝墓地在基地右边的蓝龙巢穴买传送，魔帝门徒有几率将你秒杀）任务10：追随者接受地点：无任务过程：任意难度击败魔帝之子绝天，获得他的效忠，神墓增加守卫者。击败绝天获得【天绝忘死录】任务11：半神之力接受地点：冰玄煞任务过程：成为半神后携带【贯天穿地-真】去找冰玄煞触发对话，然后将魔帝之子爆出的【天绝忘死录】交给他，获得【信物】。持有信物接近守墓老人，有几率领悟半神法则，失败后死亡（等级不下降）任务12：神墓四血卫接受地点：守墓老人身边的血饮

神之墓地攻略

神之墓地2.6a的英雄是需要随机出来的，这个有点蛋疼，我随机了好几次都没随机到，哭。废话就少说了，直接跟大家说说神之墓地2.6的打法及注意事项吧。通关主要是看你能守住家不，BOSS不难，难的是小怪，前期比较难守的是6波和9波以后的魔免怪，守的时候不能有地狱火去抗，要买骷髅杖招骷髅去抗，自己在后面打，守住这些了，后面就好守了，前2个BOSS，杀的时候最好用地狱火砸他，因为砸的时候是带晕的，BOSS基本都是晕到死的，不咋又人皇的沉默也好，只要前面2个BOSS打了后面就简单了。右下角灵兽爆灵丹，河道螃蟹爆治疗之手，左边河道上边妖皇爆浩劫，妖皇令，妖皇骨灰，妖皇下面，食尸鬼巫师爆致命毒素可以合毒素球，最左边的中间，小怪爆厄运，封魔石，领主爆曙光，镇灵石，地狱火爆命运，魂之碎片，小阿爆，永恒诅咒，魄之碎片，往右边点，火凤凰爆幽冥鬼火，上面，英雄区，昊天爆空间之刃，作者爆，绝世凶器，冰魂，右边河道，上去点，绝天爆天书，再右边，蓝龙爆龙盾，红龙爆龙晶，黑龙爆龙之号角，黄龙爆龙符，绿龙爆生生不息，再往上去点左边，守护者爆星辰书，加基地5000防的，冰爷爷爆魔杖。传送，贯穿，不用说了吧裂天=传送真+贯穿真+神力结晶苍穹=传送真+空间之刃+昊天的心脏(任务) 魔化浩劫=浩劫+妖皇骨灰丧魂龙刀=龙之号角+龙族至宝幽冥鬼爪=剑魂+幽冥鬼火+粉碎剑魂妖龙号角=龙之号角+妖皇骨灰，(上山打老虎合) 其他的装备都买的到了。任务1，传说魄之力量，去找昊天觉醒(让他杀)有几率的，觉醒了，去训练1房间的下面找那个女人，有几率触发任务的，再去杀昊天一定要把空间刃爆出来，然后在12-13点去找昊天，然后回到那女人那，昊天叫你找他的心脏，然后带神力结晶(守墓老人获得)，满地图，找心脏了，找到了永囚禁锢他，然后去找昊天，苍穹就有了。任务2，带贯穿真，杀了绝天拿，绝天爆的天书，找冰爷爷，他给你信物，然后杀守护者爆星辰书，去找守墓老人，成了真半神，把星辰书给守墓老人了，找血饮，他给你个布娃娃，带个浩劫，骨灰，布娃娃，去找隐龙，魔化浩劫了，就在隐龙旁边找忘尘，任务就完了。

神之墓地.D简单图文攻略

目录灰烬勋章（得到灰烬勋章） (2) 鼻涕纸任务（增加英雄等级任务） (4) 六慌大阵（为基地增加5000防御） (5) 法则任务（得到信物→转成真半神） (7) 魔帝与妖皇的仇怨（浩劫-妖魔化=浩劫+妖皇的灵魂→魔帝面前自动合成） (9) 四血卫（召唤血饮、忘尘、涅凡尘） (11) 无邪恋碟（妖皇变成中立） (14) 妖化龙皇号角（妖龙号角=妖皇令+妖皇的骨灰+龙皇号角→上山打老虎处触发任务） (17) 昊天剧情任务（得到皓月苍穹武器） (18) 守墓老人的试练（转身） (22) 成为准神的办法 (24) 成为真神的办法（需要天书地卷+天书下卷+天书天卷+天书人卷） (24) 复活玄缘（控制玄冥） (24) 神之墓地装备大全2.6A（物品及出处） (27) 商店物品 (27) 怪物爆出的物品及出处 (32) 需要升级合成的装备及出处 (35) 物品和任务所需物品及出处 (40) 升级装备的物品及出处 (44) 神之墓地任务简单文字攻略及获得物品 (46) 神之墓地2.6D常用指令 (49)

全图解析灰烬勋章（得到灰烬勋章）先去杀了这个怪物

它会爆出食人魔血液带着食人魔血液去找基地左侧红色熊猫NPC 然后它会给你灰烬勋章，杀500只怪涨白字属性（注：有几率得不到你多拿几次就可以了）

鼻涕纸任务（增加英雄等级任务）首先杀狂暴野兽然后得到鼻涕纸在带这鼻涕纸去找基地右侧小小熊猫NPC

注：鼻涕纸要放在第六格才有效六慌大阵（为基地增加5000防御）先杀了守护者

他会爆出六慌引辰然后带着六慌引辰去找守墓老人就会触发大阵帮基地加5000防御

神之墓地3.0.4隐藏全攻略

1.龙神任务，250级后找迷觉醒龙魂，获得全图减少35%攻击、移动、速度的光环。 2.半神之力，200级后找守墓老人对话，可获得死神怨念守墓老人死亡（绝对是装死！），然后带上死神怨念找骷髅啰嗦一大堆，玩家携带神之残魂再找骷髅就可半神。 3.毁灭前夕（龙神），400级后击败血息，可得知世界将毁灭的消息，而血息知道庇护所的位置，之后血息变中立，世界毁灭后龙族幸存。 4.毁灭前夕，击败逍遥子获得剑意·无始，并得知世界将毁灭的消息，半神后携带剑意·无始击败青冥子可获得剑意·无终，获得2个剑意，35波之后击杀阴浊，无限冰龙之时与逍遥子对话，并得知击杀冰封魔帝会获得一线生机。 5.魔帝佩剑霜寒淬，玩家半神250级后携带霜寒淬5级，与墓地左下的神之幽魂对话，之后击杀墓地右上的背叛者，获得霜寒淬，带着霜寒淬再与幽魂对话得知宝剑剑魂已失，需重铸剑魂，拿着2个剑意加剑合成神器。

6、隐藏任务不知道怎么做，任务做完第二结局。镇族之宝加龙之契约加神之残魂自动合成远古头颅。这图的超级神器，别怀疑。很牛，死亡7秒复活，后期杀青冥子必备，每秒百分之10回血、200万血，百分之75全属性。远程卡位虐逍遥，近战无敌技能杀，没无敌技能就别来找虐了，除非高属性邪帝30输出。另外，击败逍遥子会获得剑意，之外还有一个物品，逍遥战袍和美人韵之中的一个，都是极品神器，美人韵触发效果伤害极高，有了逍遥战袍就能完抗血息，这等极品装备只能得其一，渣渣神死。拿了剑意和逍遥或美人韵就去虐血息，插血棒子砸地狱火能杀死，血息会爆妖龙战甲、神之残魂、血之护符，龙神以外的英雄带着神之残魂找骷髅半神。半神后携带无始剑意击败青冥子可获得剑意·无终。本人酷爱斧头，斧头这图永远的最强，无限刷绝天爆龙之契

神之墓地攻略

找骷髅半神。半神后携带无始剑意击败青冥子可获得剑意·无终。本人酷爱斧头，斧头这图永远的最强，无限刷绝天爆龙之契约卖木材，一个就可以买3个9999白字攻击药水，刷到200万白字攻击，技能加成百分之1000伤害，这时你会发现你无敌了，开启10秒无敌爆击一次没有秒杀不了的怪。2.7的任务大部分都是隐藏的，需要玩家自己去触发！昊天任务：1.传送到没落的龙族哪里，找到小霜儿，触发对话，得到水晶球一个;(元力需要23以上) 2.到森林迷宫找到昊天（其实是转世之魂），触发对话，得到一封信，并打开城门（城门在强盗头子右上） 3.进入四海城，找到小霜儿，触发对话，失去水晶球，打开赢霜的城门，找到赢霜，得到空间之刃（玩家就可以灰来灰去了）

神之墓地隐藏全攻略图文稿

神之墓地隐藏全攻略集团文件发布号：（9816-UATWW-MWUB-WUNN-INNUL-DQQTY-

5.魔帝佩剑霜寒淬，玩家半神250级后携带霜寒淬5级，与墓地左下的神之幽魂对话，之后击杀墓地右上的背叛者，获得霜寒淬，带着霜寒淬再与幽魂对话得知宝剑剑魂已失，需重铸剑魂，拿着2个剑意加剑合成神器。 6、隐藏任务不知道怎么做，任务做完第二结局。镇族之宝加龙之契约加神之残魂自动合成远古头颅。这图的超级神器，别怀疑。很牛，死亡7秒复活，后期杀青冥子必备，每秒百分之10回血、200万血，百分之75全属性。远程卡位虐逍遥，近战无敌技能杀，没无敌技能就别来找虐了，除非高属性邪帝30输出。另外，击败逍遥子会获得剑意，之外还有一个物品，逍遥战袍和美人韵之中的一个，都是极品神器，美人韵触发效果伤害极高，有了逍遥战袍就能完抗血息，这等极品装备只能得其一，渣渣神死。

拿了剑意和逍遥或美人韵就去虐血息，插血棒子砸地狱火能杀死，血息会爆妖龙战甲、神之残魂、血之护符，龙神以外的英雄带着神之残魂找骷髅半神。半神后携带无始剑意击败青冥子可获得剑意·无终。本人酷爱斧头，斧头这图永远的最强，无限刷绝天爆龙之契约卖木材，一个就可以买3个9999白字攻击药水，刷到200万白字攻击，技能加成百分之1000伤害，这时你会发现你无敌了，开启10秒无敌爆击一次没有秒杀不了的怪。

《神之墓地》斧狂逆天打法图文攻略

开局小鸟买个地狱火丢右下，英雄买个鞋子跑到右下，鸟用完就丢英雄，英雄用完后再丢仓库，这样就有3个地狱火了，出2个金币后合个盾再买个地狱火，重复上面步骤就有6个地狱火了，盾和地狱火给仓库拿。英雄HG然后-H，自己跑去浮生那，就带个鞋子就行了，放R然后E，鸟注意拿金币，够3W后买个盾个地狱火一直刷右下。快的话1波快到基地仓库的地狱火CD就好了，然后丢去守家，怪多起来后英雄HG，然后放R慢慢砍，够木就买爪子。英雄到25后去杀螃蟹..先丢地狱火然后放R砍.. 英雄到40多(我是44)用纸升到50，然后去刷胖子，跑到那后开E然后T，RP好一次就出了。鸟一直刷右下和卖晶石的话这时候绝对有100木了，然后出MAX戒指给英雄，这时候T还在持续时间中，所以花1W去钱房然后杀内丹，高级地狱火是左下一只，右下2只。

英雄50CD好了后花20木买隐身，然后再花10木去石头房，先放E然后T，E 没了他们也死了(如果你死了那是你技术不行)，留1个魂其他全卖。英雄守家到100，100后可以刷钱房到50CD恢复，50CD恢复后再去石头房，刷的方法同上，不过要找怪多的地方，石头全卖因为你前面留魂了，然后鸟合传说，木多的话再出个MAX戒指给鸟自己带。合出剑的时候一般是晚上，带盾和地狱火进，然后用地狱火晕，RP好的话不需要鸟或仓库帮丢，然后去刷下面那个，英雄站旁边等地狱火CD，然后-H，鸟也一起来，6次晕RP再差也能全灭了。英雄花20木买隐身然后跑到昊天门前-H，仓库丢地狱火，英雄再跑到小啊那，站他后面，鸟丢地狱火英雄一直砍，RP好出2个碎骨就秒了。

英雄跑到仓库那，一起丢地狱火，6个左右就够了，拿1个去引昊天，其他的逃跑，他追过来后攻击他，他会分身然后发呆，这时候丢2个地狱火再去引过来，英雄放T站门前，这时候他会追过来，然后分身，一般不会出门，等第2次就有几个会出来。这时候你一定死了，复活后买个隐身跑到他旁边然后用E，RP不是太差10秒绝对觉醒，然后去练级房1号去撞水晶，得到水晶后带个MAX爪去刷木。刷到10:30左右，你也可以提前去，10:30的时候HG然后买隐身站门口，等12点就交任务，得元神后把传说给他加满蓝，然后去刷4只龙，自己有镇族后就去A黑龙，没血了就跑，RP好可以不死。够1505木后帮元神买个聚能，然后去杀绝天，杀完绝天杀老人，1个碎骨可以打70%，妖皇也是，磨的时候记得刷4龙，老人死后给聚能给英雄，英雄飞过去拿仗，拿完后再还给元神，然后元神杀妖皇，也可以先出贯穿，然后把浩劫给英雄刷到贯穿妖化。

神之墓地2.6c攻略

神之墓地2.6c攻略（一）守墓老人的恐怖试炼 *********************** 这个神秘的老人自从神墓诞生之时开始就守护着神墓，他把握着神灵气力的秘密。冰封魔帝以为他实在已经超越了神灵，但是怎么看，他都只是一个行将就木的老头子。在守墓老人看来，一个修炼者能否达到半神的境界，关键是看个人的意志力，而先天的条件并不重要。任务过程：英雄携带一个“心之结晶”接近守墓老人。 90%几率死亡、等级下降10级。 10%几率得到守墓老人的认可，获得其赠予的神力结晶。同时守墓老人将消失。 *********************** （二）小熊猫的烦恼 *********************** 小熊猫是熊猫族里最为强大的战士之一。他最为骄傲的便是他能打造出各种神奇无比的装备。但是他是个很希奇的熊猫，有时很大方有时却很吝啬。任务过程：为小熊猫找些血液。运气好，你会发现他很大方的给你一个神奇的装备。运气差，你会郁闷的得到“不够，多拿些来”这种气人的回答。获得物品：【耶稣的十字架】 ********************** （三）小小熊猫的烦恼 ********************** 小小熊猫是熊猫族里最令人头痛的熊猫了，他整天思考着一些无聊透顶的题目，但是他和熊猫老大有个相同的嗜好。他们都喜欢收集一些稀奇古怪的玩意。任务过程：到野兽领地***野兽。得到的鼻涕纸给予小小熊猫。任务奖励：提升等级。 ********************** （四）胖子的恶心嗜好 ********************** 胖子到底是谁生的谁也回答不上来。很难想象世界上居然有如此丑陋的人物。让人佩服的是他老妈居然没有活生生把他掐死。这个丑陋的家伙心里严重***、看任何人都不爽、喜欢吃各种心脏。任务过程：到食人魔领地猎杀食人魔。得到的食人魔心脏给予胖子。任务奖励：心之结晶。 ********************** （五）小禽兽的猥琐心里 ********************** 小禽兽帅得一塌糊涂、糟践美女无数，而且一生的梦想就是泡尽天下美女。最近又看上了人皇，奈何人皇心有所属根本不鸟他。人皇可以借此色诱小禽兽。任务过程：采集50朵“好大一颗花”，等级达到150后接近小禽兽，和小禽兽对话。

神之墓地2.6c攻略

【百度文库核心用户上传】神之墓地 2.6c攻略（一）守墓老人的恐怖试炼 *********************** 这个神秘的老人自从神墓诞生之时开始就守护着神墓，他把握着神灵气力的秘密。冰封魔帝以为他实在已经超越了神灵，但是怎么看，他都只是一个行将就木的老头子。在守墓老人看来，一个修炼者能否达到半神的境界，关键是看个人的意志力，而先天的条件并不重要。任务过程： xx携带一个“心之结晶”接近守墓老人。 90%几率死亡、等级下降10级。 10%几率得到守墓老人的认可，获得其赠予的神力结晶。同时守墓老人将消失。 *********************** （二）xx的烦恼 *********************** 小熊猫是熊猫族里最为强大的战士之一。他最为骄傲的便是他能打造出各种神奇无比的装备。但是他是个很希奇的熊猫，有时很大方有时却很吝啬。任务过程：为小熊猫找些血液。运气好，你会发现他很大方的给你一个神奇的装备。运气差，你会郁闷的得到“不够，多拿些来”这种气人的回答。获得物品：

【xx的十字架】 ********************** （三）小xx的烦恼 ********************** 小小熊猫是熊猫族里最令人头痛的熊猫了，他整天思考着一些无聊透顶的题目，但是他和熊猫老大有个相同的嗜好。他们都喜欢收集一些稀奇古怪的玩意。任务过程：到野兽领地***野兽。得到的鼻涕纸给予小小熊猫。任务奖励：提升等级。 ********************** （四）胖子的恶心嗜好 ********************** 胖子到底是谁生的谁也回答不上来。很难想象世界上居然有如此丑陋的人物。让人佩服的是他老妈居然没有活生生把他掐死。这个丑陋的家伙心里严重***、看任何人都不爽、喜欢吃各种心脏。任务过程：到食人魔领地猎杀食人魔。得到的食人魔心脏给予胖子。任务奖励：心之结晶。 **********************

《神之墓地》妖灵单通心得攻略

《神之墓地》妖灵单通心得攻略有人说妖灵的老虎后期很弱，想要作者加强，这是个很奇怪的问题。妖灵的老虎在前期的表现难道你看不见，后期弱，如果老虎后期也能抗怪的话，你觉得妖灵还有玩下去的意义吗？人物不停的刷资源，基本都不需要管家，这样的地图，你还有信心继续玩下去吗，如果老虎后期也能抗怪，试问和盗版有何区别。个人感觉妖灵很厉害的，出资源不比任何一个英雄慢，娜迦之前根本不需要操心基地。而且最重要的是造型真好看，感觉魔兽里最正常的人物就是她了，其他的都人不人鬼不鬼的。开局选人，买邪恶和地狱火，RT红圈那里，人仍了地狱火之后给小鸟拿，然后小鸟去中间砸地狱火，丢下仓库去打血液。这里有个需要注意的是，仓库仍地狱火的范围，扔了地狱火之后最好把地狱火往右边控制走点。

人过去刷血液最多二次暴风雪，就应该７级了吧，召唤老虎去红圈那里，然后小鸟砸地狱火破灵兽无敌。人交了血液得十字架，然后去胖妞那里买二邪恶三毒液，然后呆武器店那里，先锋来基地的时候，你内丹也应该出了。需要注意的是灵兽无敌之后的时间，怎么说吧，如果你晚了，基地就无敌了，或者灵兽的无敌技能就好了。出了内丹的时候，召唤老虎，拉一只老虎回去打先锋，然后吃内丹，老虎的攻击和英雄的属性和有关。吃了内丹属性应该是８００左右吧，老虎看家毫无压力，或许有人说，就算不吃内丹老虎看家也无压力吧。

怎么说吧，个人感觉妖灵的玩法虽然挺多，不过１波前出内丹的这个方法是最有效，也是最快出资源的方法吧。需要注意的是，老虎打先锋不要一起去，先锋的技能可不是老虎能抗的。先锋死了之后，人就可以去练级房刷十字了，二只老虎看家，三只老虎出毒素，刷十字的时候注意站位就行了。站那里ｈ，站好位置之后，RT红圈那里仍地狱火，旁边练级房那里仍个地狱火开视野。红圈那里仍地狱火是二波怪之后三波的火枪手，把地狱火仍红圈那里，旁边房间的怪会跑过来打红圈那里的地狱火。暴风雪的范围刚好够你刷二边怪，三波怪完毕，估计最少应该有90多级了吧，拿上鼻涕去交任务吧，拿上贯穿去打石头吧。

神之墓地攻略(本剧情由帝上小明提供)(请用word程序打开)

(本剧情由帝上[小明]所提供) 剧情最好物品栏空一个才做，产生不良效果不要怨我！ 1.75级前往守墓老人处(选英雄下面) 2.100级带着死神怨念(守墓老人给你的)去白骨法师处. 3.125级带着神之残魂(血息有几率掉)再次前往 1.击败绝天即可获得。 1.携带天决忘情录前往天决处即可 1.半神后并且80级（这等级是废话好不）携带霜寒淬[5/5]去冥河娃娃处。 2.击败巫妖【在偷袭怪那边】。（注意，巫妖是隐身的，要携带神力结晶） 3.再次前往冥河娃娃那。（这步基本上不用做） 1.击败逍遥子。 2.半神后携带剑意·无始击败青冥子获得剑意·无终 3.200级并且36波前往逍遥子处获得盘龙戒和魔剑 1.龙神变身后并且没有准神和等级大于90前往迷处(迷在树人左下角处) 2.100级击败妖龙血息 1.半神后前往君无邪处(在四海城) 2.半神并且等级大于100级和携带净化浮雕前往妖皇处 3.半神并且等级大于100级和携带净化浮雕前往君无邪处

1. 携带浩劫-碎片和妖皇令前往隐龙处 1.携带虚天刃并且等级大于125级被昊天打有一定几率触发剧情 2.等级大于140前往小赢霜处(在龙那) 3.等级大于140前往昊天处 4.携带水晶球去四海城护法那(蓝色的) 5.携带传说之剑前往赢霜那 6.携带水晶球去小赢霜那(赢霜左边)[这两步可以先做赢霜那然后走到小赢霜那以前] 7.去昊天那(这个昊天不是第一步的昊天,在门口的右边) 8.180级去第一步的昊天那,获得传说之剑-觉醒 9.击败扎魔(在四海城入口左边的湖深处)获得空间之刃 10.等级大于250并且携带传说之剑-觉醒和空间之刃去昊天那(这个昊天在赢霜右边) 1.半神后无限循环接近玄清即可 1.半神后并且等级大于215前往灵处（地图右下角）（他会给你个天书） 2.使用天书（若失败，减少等级和属性） 1.准神后前往冰玄煞那（在基地左上角的建筑前往） 1.准神后携带神格前往白骨法师处 2.携带神格、厚土甲、冰封球、烈焰扇以及妖皇令前往白骨法师处等待180秒即可获得 1.等级大于300并且携带霜寒淬和剑意·无始和剑意·无终前往隐龙处（基地左上角建筑购买进入） 1.等级大于350携带霜寒淬-无始无终和皎月苍穹前往神死魔灭处

神之墓地3.0.4隐藏全攻略

经过一番的周折，在此为大家送上神之墓地3.0.4隐藏全攻略： 1.龙神任务，250级后找迷觉醒龙魂，获得全图减少35%攻击、移动、速度的光环。 2.半神之力，200级后找守墓老人对话，可获得死神怨念守墓老人死亡（绝对是装死！），然后带上死神怨念找骷髅啰嗦一大堆，玩家携带神之残魂再找骷髅就可半神。 3.毁灭前夕（龙神），400级后击败血息，可得知世界将毁灭的消息，而血息知道庇护所的位置，之后血息变中立，世界毁灭后龙族幸存。 4.毁灭前夕，击败逍遥子获得剑意·无始，并得知世界将毁灭的消息，半神后携带剑意·无始击败青冥子可获得剑意·无终，获得2个剑意，35波之后击杀阴浊，无限冰龙之时与逍遥子对话，并得知击杀冰封魔帝会获得一线生机。 5.魔帝佩剑霜寒淬，玩家半神250级后携带霜寒淬5级，与墓地左下的神之幽魂对话，之后击杀墓地右上的背叛者，获得霜寒淬，带着霜寒淬再与幽魂对话得知宝剑剑魂已失，需重铸剑魂，

拿着2个剑意加剑合成神器。 6、隐藏任务不知道怎么做，任务做完第二结局。镇族之宝加龙之契约加神之残魂自动合成远古头颅。这图的超级神器，别怀疑。很牛，死亡7秒复活，后期杀青冥子必备，每秒百分之10回血、200万血，百分之75全属性。远程卡位虐逍遥，近战无敌技能杀，没无敌技能就别来找虐了，除非高属性邪帝30输出。另外，击败逍遥子会获得剑意，之外还有一个物品，逍遥战袍和美人韵之中的一个，都是极品神器，美人韵触发效果伤害极高，有了逍遥战袍就能完抗血息，这等极品装备只能得其一，渣渣神死。拿了剑意和逍遥或美人韵就去虐血息，插血棒子砸地狱火能杀死，血息会爆妖龙战甲、神之残魂、血之护符，龙神以外的英雄带着神之残魂找骷髅半神。半神后携带无始剑意击败青冥子可获得剑意·无终。

神之墓地隐藏全攻略完整版

神之墓地隐藏全攻略 HEN system office room 【HEN16H-HENS2AHENS8Q8-HENH1688】

淬，带着霜寒淬再与幽魂对话得知宝剑剑魂已失，需重铸剑魂，拿着2个剑意加剑合成神器。 6、隐藏任务不知道怎么做，任务做完第二结局。镇族之宝加龙之契约加神之残魂自动合成远古头颅。这图的超级神器，别怀疑。很牛，死亡7秒复活，后期杀青冥子必备，每秒百分之10回血、200万血，百分之75全属性。远程卡位虐逍遥，近战无敌技能杀，没无敌技能就别来找虐了，除非高属性邪帝30输出。另外，击败逍遥子会获得剑意，之外还有一个物品，逍遥战袍和美人韵之中的一个，都是极品神器，美人韵触发效果伤害极高，有了逍遥战袍就能完抗血息，这等极品装备只能得其一，渣渣神死。

神之墓地攻略(全)

携带【传说之剑-魄之力量】时被昊天攻击，有几率觉醒为【传说之剑-真】任务8：贯穿天地的妖化接受地点：无任务过程：持有【贯穿天地-永恒诅咒】后，杀死任意敌人有几率妖化为【贯穿天地-真】（几率低下，需大规模刷怪）任务9：妖皇与魔帝的xx 接受地点：无任务过程：携带【深渊魔甲MAX】和【妖皇的骨灰】进入魔帝墓地，魔帝的灵魂将给【深渊魔甲MAX】注入魔气，获得物品【深渊魔甲-魔化】（魔帝墓地在基地右边的蓝龙巢穴买传送，魔帝门徒有几率将你秒杀）任务10：追随者接受地点：无任务过程：任意难度击败魔帝之子绝天，获得他的效忠，神墓增加守卫者。击败绝天获得【天绝忘死录】任务11：半神之力接受地点： xx煞任务过程：成为半神后携带【贯天穿地-真】去找冰玄煞触发对话，然后将魔帝之子爆出的【天绝忘死录】交给他，获得【信物】。持有信物接近守墓老人，有几率领悟半神法则，失败后死亡（等级不下降）任务12：神墓四血卫

神之墓地2.8b详细攻略

可选三个游戏模式：【菜鸟】：有诸多的彩蛋，不喜玩高手以上。“娱乐至上”召唤bb波数7-17。小鸟可以t 神死雕像获得附件一个额外单位传送。出怪汇集口左右两边砸树大概率出彩蛋。难度90以上赤火石像和祖龙获得魔帝回血光环。可以自选天赋，看自己想要的天赋在祭坛的位置，1是剑圣，2是怨女，所以-tfhq1无敌斩，-tfhq2幽冥。无法开启第二结局，无法开启先锋特殊怪。虎哥会复活。虎哥死亡掉落物品概率大大提高。难度可调整1-100。【高手】：除了大治疗和小闪烁，禁用一切彩蛋。可以双天赋，不能自选，可以手动开启先锋特殊怪。最低难度20。【大婶】：同高手禁用彩蛋，只能单天赋，自动开启先锋特殊怪。最低难度60，送难度-50 的木头。以后高手大婶们不用再嫌弃娱乐模式了，因为更名菜鸟模式了，大家都懂得什么意思。常规剧情任务：守护神之墓地，阻止冰封势力，杀死冰封魔帝。守家：胖妞那里接。绝天：杀死绝天帮你守家。半神：熊猫买书，可吃可领悟。吃了无属性等级加成。六荒法阵&妖弓任务：半神以后找守墓老人。六荒大蛇无敌解除，杀死掉落六荒引辰交给守墓老人，基地加防御5000。人物会获得神力结晶，提示你带结晶找冰凌他爷，在地图最右上方冰火岛。激活妖弓任务和寻找四血卫任务。贯穿妖化：任务触发以后，英雄携带贯穿天地max杀敌有概率妖化，概率公式：1/(难度等级*10+玩家数*200+500)。四血卫：妖弓任务触发以后，会提示xxx有什么xxx气息，就是带神力去六荒下边找破虚。杀死破虚，破虚投奔魔帝，10波后进攻墓地。绝天获得物品栏，5万三围奖励。血饮忘尘回家当奶妈。聂凡尘：破虚进攻墓地，如果绝天没有天书人卷就会被虐。所以最好提前激活聂凡尘，迎接破虚的到来。当然带人卷，绝天7万左右防御，可以裸奔抗破虚。激活聂凡尘需要杀6次幽冥凤凰，给聂凡尘6个蛋，他就回家了。破虚遇到开启凤凰血脉的聂凡尘后，不屈魂魄